1
|
Goldfarb G, Sela Y. The Ideal Diet for Humans to Sustainably Feed the Growing Population - Review, Meta-Analyses, and Policies for Change. F1000Res 2023; 10:1135. [PMID: 37928317 PMCID: PMC10623543 DOI: 10.12688/f1000research.73470.1] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Figures] [Journal Information] [Submit a Manuscript] [Subscribe] [Scholar Register] [Accepted: 05/26/2023] [Indexed: 11/07/2023] Open
Abstract
INTRODUCTION As of now, no study has combined research from different sciences to determine the most suitable diet for humans. This issue is urgent due to the predicted population growth, the effect of this on the environment, and the deterioration of human health and associated costs. METHODS A literature review determined whether an optimal diet for humans exists and what such a diet is, followed by six meta-analyses. The standard criteria for conducting meta-analyses of observational studies were followed. A review of literature reporting Hazard Ratios with a 95% confidence interval for red meat intake, dairy intake, plant-based diet, fiber intake, and serum IGF-1 levels were extracted to calculate effect sizes. RESULTS Results calculated using NCSS software show that high meat consumption increases mortality probability by 18% on average and increases diabetes risk by 50%. Plant-based and high-fiber diets decrease mortality by 15% and 20% respectively ( p < .001). Plant-based diets decreased diabetes risk by 27%, and dairy consumption (measured by increased IGF-1 levels) increased cancer probability by 48% ( p < 0.01). A vegetarian or Mediterranean diet was not found to decrease the probability of heart disease. A vegetarian diet can be healthy or not, depending on the foods consumed. A Mediterranean diet with high quantities of meat and dairy products will not produce the health effects desired. The main limitations of the study were that observational studies were heterogeneous and limited by potential confounders. DISCUSSION The literature and meta-analyses point to an optimal diet for humans that has followed our species from the beginnings of humankind. The optimal diet is a whole food, high fiber, low-fat, 90+% plant-based diet. This diet allowed humans to become the most developed species on Earth. To ensure people's nutritional needs are met healthily and sustainably, governmental dietary interventions are necessary.
Collapse
Affiliation(s)
- Galit Goldfarb
- Nutrition, OUS University, The Royal Academy of Economics and Technology, Zürich, Switzerland
| | - Yaron Sela
- Nutrition, OUS University, The Royal Academy of Economics and Technology, Zürich, Switzerland
| |
Collapse
|
2
|
Fannin LD, Swedell L, McGraw WS. Enamel chipping and its ecological correlates in African papionins: Implications for hominin feeding behavior. J Hum Evol 2023; 177:103330. [PMID: 36898301 DOI: 10.1016/j.jhevol.2023.103330] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/06/2022] [Revised: 01/23/2023] [Accepted: 01/25/2023] [Indexed: 03/12/2023]
Abstract
African papionins are classic paleoecological referents for fossil hominins. Enamel chips on the teeth of baboons and hominins are argued to represent responses to similar dietary habits; however, a comprehensive analysis of modern papionin chipping is lacking, leaving open the question of analog suitability. Here, we investigate patterns of antemortem enamel chipping across a diverse set of African papionin species occupying a range of ecological niches. We compare papionin chipping frequencies to estimates for Plio-Pleistocene hominins to address hypotheses of habitat and/or dietary similarities. Antemortem chips in seven African papionin species were scored on intact postcanine teeth (P3-M3) using established protocols. Chip size was scored on a tripartite scale. Papio hamadryas and Papio ursinus-two common paleoecological referents-display higher levels of chipping than Plio-Pleistocene hominin taxa (Australopithecus and Paranthropus) posited to have similar dietary habits. Papio populations occupying dry or highly seasonal habitats accumulate more large chips than Papio taxa occupying more mesic habitats, and terrestrial papionins chip their teeth more often than closely related taxa occupying arboreal niches. Chipping is present on the teeth of all Plio-Pleistocene hominins; however, chipping in baboons (P. ursinus and P. hamadryas) consistently exceeds most hominin taxa. Chipping frequencies on their own do not reliably sort taxa into major dietary groupings. We conclude that the large differences in chipping frequency may instead reflect habitat use and food processing idiosyncrasies. Less chipping in Plio-Pleistocene hominin teeth compared to modern Papio is more likely attributable to differences in dental morphology rather than diet.
Collapse
Affiliation(s)
- Luke D Fannin
- Department of Anthropology, Dartmouth College, Hanover, NH, 03755, USA; Graduate Program in Ecology, Evolution, Environment, and Society, Dartmouth College, Hanover, NH, 03755, USA.
| | - Larissa Swedell
- Department of Anthropology, Queens College, City University of New York, Flushing, NY, 11367, USA; Anthropology Program, Graduate Center, City University of New York, New York, NY, 10016, USA; New York Consortium in Evolutionary Primatology, New York, NY, 10016, USA; Department of Archaeology, University of Cape Town, Rondebosch, Western Cape, 7700, South Africa
| | - W Scott McGraw
- Department of Anthropology, The Ohio State University, Columbus, OH, 43210, USA
| |
Collapse
|
3
|
O'Brien K, Hebdon N, Faith JT. Paleoecological evidence for environmental specialization in Paranthropus boisei compared to early Homo. J Hum Evol 2023; 177:103325. [PMID: 36805971 DOI: 10.1016/j.jhevol.2023.103325] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/13/2022] [Revised: 01/15/2023] [Accepted: 01/16/2023] [Indexed: 02/18/2023]
Abstract
Since the discovery of Paranthropus boisei alongside early Homo at Olduvai Gorge and East Turkana, paleoanthropologists have attempted to understand the different evolutionary paths of these two hominin lineages. Conventional wisdom is that their prolonged phase of sympatry in eastern Africa reflects different adaptive strategies, with early Homo characterized as the ecologically flexible generalist and Paranthropus as the less versatile specialist. If correct, this should imply differences in their use of ancient environments, with early Homo occurring in a broader range of environmental contexts than Paranthropus. This prediction has yet to be subject to rigorous quantitative evaluation. In this study, we use the 2.0-1.4 Ma fossil bovid assemblages associated with early Homo and P. boisei at East Turkana (Kenya) to quantify the breadth of their environmental associations. We find that early Homo occurs in faunal assemblages indicative of a broader range of environments than P. boisei. A null model taking sampling into account shows that the broad environmental associations of early Homo are indistinguishable from random, whereas P. boisei is one of just a handful of large mammal taxa from East Turkana that has a narrower range of environmental associations than expected by chance. These results support the characterization of P. boisei as an ecological specialist relative to the more generalist Homo. Moreover, the narrow environmental associations observed of P. boisei, unlike those of almost all other C4 grass-consumers in the Turkana Basin, suggest that it likely did not feed on a spatially widespread C4 resource like the leaves, seeds, or rhizomes of grass.
Collapse
Affiliation(s)
- Kaedan O'Brien
- Department of Anthropology, University of Utah, 260 South Central Campus Drive, Salt Lake City, UT 84112, USA; Natural History Museum of Utah, University of Utah, 301 Wakara Way, Salt Lake City, UT 84108, USA.
| | - Nicholas Hebdon
- Department of Biological Sciences, Chapman University, 1 University Dr, Orange, CA 92866, USA
| | - J Tyler Faith
- Department of Anthropology, University of Utah, 260 South Central Campus Drive, Salt Lake City, UT 84112, USA; Natural History Museum of Utah, University of Utah, 301 Wakara Way, Salt Lake City, UT 84108, USA; Origins Centre, University of the Witwatersrand, 1 Jan Smuts Avenue, Braamfontein 2000, Johannesburg, South Africa
| |
Collapse
|
4
|
Ramírez-Pedraza I, Martínez LM, Aouraghe H, Rivals F, Tornero C, Haddoumi H, Estebaranz-Sánchez F, Rodríguez-Hidalgo A, van der Made J, Oujaa A, Ibáñez JJ, Mhamdi H, Souhir M, Aissa AM, Chacón MG, Sala-Ramos R. Multiproxy approach to reconstruct fossil primate feeding behavior: Case study for macaque from the Plio-Pleistocene site Guefaït-4.2 (eastern Morocco). Front Ecol Evol 2023. [DOI: 10.3389/fevo.2023.1011208] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/04/2023] Open
Abstract
The genus Macaca belongs to Cercopithecidae (Old World monkeys), Cercopithecinae, Papionini. The presence of Macaca in North Africa is well known from the Late Miocene to the Late Pleistocene. However, the diet of fossil Macaca has been poorly described in the literature. In this study, we investigated the feeding habits of Macaca cf. sylvanus (n = 4) from the Plio-Pleistocene site Guefaït-4.2 in eastern Morocco through multiproxy analysis combining analyses of stable carbon and oxygen isotopes from tooth enamel, buccal microtexture, and low-magnification occlusal dental microwear. For both microwear analyses, we compared the macaques with a new reference collection of extant members of Cercopithecoidea. Our occlusal microwear results show for the fossil macaque a pattern similar to the extant Cercocebus atys and Lophocebus albigena, African forest-dwelling species that are characterized by a durophagous diet based mainly on hard fruit and seed intake. Buccal microtexture results also suggest the consumption of some grasses and the exploitation of more open habitats, similar to that observed in Theropithecus gelada. The δ13C of M. cf. sylvanus indicates a C3 based-diet without the presence of C4 plants typical of the savanna grassland in eastern Africa during this period. The high δ18O values of M. cf. sylvanus, compared with the contemporary ungulates recovered from Guefaït-4.2, could be associated with the consumption of a different resource by the primate such as leaves or fresh fruits from the upper part of trees. The complementarity of these methods allows for a dietary reconstruction covering a large part of the individual’s life.
Collapse
|
5
|
Paine OCC, Daegling DJ. The game of models: Dietary reconstruction in human evolution. J Hum Evol 2023; 174:103295. [PMID: 36521317 DOI: 10.1016/j.jhevol.2022.103295] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/15/2022] [Revised: 10/28/2022] [Accepted: 11/01/2022] [Indexed: 12/15/2022]
Abstract
Despite substantial additions to the paleontological record and unanticipated improvements in analytical techniques since the Journal of Human Evolution was first published, consensus on the diet of early hominin species remains elusive. For instance, the notable advances in the analyses of hominin dental microwear and stable isotopes have provided a plethora of data that have in some instances clouded what was once ostensibly a clear picture of dietary differentiation between and within hominin taxa. In the present study, we explore the reasons why the retrodiction of diet in human evolution has proven vexing over the last half century from the perspective of both ecological and functional-mechanical models. Such models continue to be indispensable for paleobiological reconstructions, but they often contain rigid or unstated assumptions about how primary paleontological data, such as fossils and their geological and taphonomic contexts, allow unambiguous insight into the evolutionary processes that produced them. In theoretical discussions of paleobiology, it has long been recognized that a mapping function of morphology to adaptation is not one-to-one, in the sense that a particular trait cannot necessarily be attributed to a specific selective pressure and/or behavior. This article explores how the intrinsic variability within biological systems has often been underappreciated in paleoanthropological research. For instance, to claim that derived anatomical traits represent adaptations related to stereotypical behaviors largely ignores the importance of biological roles (i.e., how anatomical traits function in the environment), a concept that depends on behavioral flexibility for its potency. Similarly, in the paleoecological context, the underrepresentation of variability within the 'edible landscapes' our hominin ancestors occupied has inhibited an adequate appreciation of early hominin dietary flexibility. Incorporating the reality of variation at organismal and ecological scales makes the practice of paleobiological reconstruction more challenging, but in return, allows for a better appreciation of the evolutionary possibilities that were open to early hominins.
Collapse
Affiliation(s)
- Oliver C C Paine
- Department of Anthropology, San Diego State University, San Diego, CA, 92182, USA.
| | - David J Daegling
- Department of Anthropology, University of Florida, Gainesville, FL, 32611, USA.
| |
Collapse
|
6
|
Fine-scaled climate variation in equatorial Africa revealed by modern and fossil primate teeth. Proc Natl Acad Sci U S A 2022; 119:e2123366119. [PMID: 35994633 PMCID: PMC9440354 DOI: 10.1073/pnas.2123366119] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
Environmental variability may have spurred unique adaptations among Miocene apes and later hominins, but this hypothesis has been impossible to test on the scale relevant to individual lifespans. We establish that oxygen isotope compositions in modern primate teeth record annual and semiannual seasonal rainfall patterns across a broad range of environments in equatorial Africa. We then document annual dry seasons experienced by the large-bodied Early Miocene ape Afropithecus turkanensis, which may explain its novel dental adaptations and prolonged development. By revealing real-time historical and prehistoric environmental variation on a near weekly basis, we demonstrate that extraordinary behavioral and ecological variability can be recovered from modern and fossil African primates. Variability in resource availability is hypothesized to be a significant driver of primate adaptation and evolution, but most paleoclimate proxies cannot recover environmental seasonality on the scale of an individual lifespan. Oxygen isotope compositions (δ18O values) sampled at high spatial resolution in the dentitions of modern African primates (n = 2,352 near weekly measurements from 26 teeth) track concurrent seasonal precipitation, regional climatic patterns, discrete meteorological events, and niche partitioning. We leverage these data to contextualize the first δ18O values of two 17 Ma Afropithecus turkanensis individuals from Kalodirr, Kenya, from which we infer variably bimodal wet seasons, supported by rainfall reconstructions in a global Earth system model. Afropithecus’ δ18O fluctuations are intermediate in magnitude between those measured at high resolution in baboons (Papio spp.) living across a gradient of aridity and modern forest-dwelling chimpanzees (Pan troglodytes verus). This large-bodied Miocene ape consumed seasonally variable food and water sources enriched in 18O compared to contemporaneous terrestrial fauna (n = 66 fossil specimens). Reliance on fallback foods during documented dry seasons potentially contributed to novel dental features long considered adaptations to hard-object feeding. Developmentally informed microsampling recovers greater ecological complexity than conventional isotope sampling; the two Miocene apes (n = 248 near weekly measurements) evince as great a range of seasonal δ18O variation as more time-averaged bulk measurements from 101 eastern African Plio-Pleistocene hominins and 42 papionins spanning 4 million y. These results reveal unprecedented environmental histories in primate teeth and suggest a framework for evaluating climate change and primate paleoecology throughout the Cenozoic.
Collapse
|
7
|
Pilbeam D, Wood B. Contingency rules. J Hum Evol 2022. [DOI: 10.1016/j.jhevol.2022.103167] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
|
8
|
Jiang Q, Zhao L, Guo L, Hu Y. First direct evidence of conservative foraging ecology of early Gigantopithecus blacki (~2 Ma) in Guangxi, southern China. AMERICAN JOURNAL OF PHYSICAL ANTHROPOLOGY 2021; 176:93-108. [PMID: 33964022 DOI: 10.1002/ajpa.24300] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/01/2020] [Revised: 03/09/2021] [Accepted: 04/09/2021] [Indexed: 12/30/2022]
Abstract
OBJECTIVES Gigantopithecus blacki, the largest hominoid known, is one of the representative Pleistocene mammals in southern China and northern Southeast Asia. Here we investigate the feeding ecology of G. blacki in its core habitat (Guangxi, Southern China) during the early Early Pleistocene, which was the early period in its evolution. MATERIALS AND METHODS The stable isotopic (C, O) analysis of tooth enamel of the fauna associated with G. blacki (n = 58), including the largest number of G. blacki teeth (n = 12) to date from the Liucheng Gigantopithecus Cave (~2 Ma), Guangxi, China, is undertaken. RESULTS The δ13 C values of Liucheng fauna range from -12.9 to -19.0‰ with an average of -16.1 ± 1.3‰ (n = 58) and the δ18 O values range from -4.3 to -9.6‰ with an average of -6.9 ± 1.2‰ (n = 58). The δ13 C values of G. blacki range from -15.9‰ to -17.0‰ with an average of -16.5 ± 0.4‰ (n = 12), and the δ18 O values vary from -5.9‰ to -7.5‰ with an average of -6.6 ± 0.5‰ (n = 12). CONCLUSIONS The isotopic data show Guangxi was characterized by closed C3 forest and humid climate in the early Early Pleistocene. Niche partitioning is found among G. blacki, Sinomastodon, Ailuropoda and Stegodon, the typical megafauna in South China in the early Early Pleistocene. This could be one of the important factors for them to co-exist until the Middle Pleistocene. Smallest isotopic variations of G. blacki are found compared with those of contemporary animals, indicating a conservative foraging ecology i.e., limited foraging area and/or narrow dietary flexibility. Furthermore, the more confined foraging ecology of G. blacki is also seen in comparison with fossil and extant large-bodied primates. However, the unique dietary pattern of G. blacki does not seem to have hindered its survival. The environment in Guangxi during the early Early Pleistocene offered the suitable conditions for G. blacki to become one of the typical species in the faunal assemblages.
Collapse
Affiliation(s)
- Quyi Jiang
- Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China.,Department of Archaeology and Anthropology, University of Chinese Academy of Sciences, Beijing, China.,Zhejiang Provincial Office of Cultural Relics Authentication, Hangzhou, China
| | - Lingxia Zhao
- Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China.,CAS Center for Excellence in Life and Paleoenvironment, Beijing, China
| | - Lin Guo
- Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China.,CAS Center for Excellence in Life and Paleoenvironment, Beijing, China.,College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, China
| | - Yaowu Hu
- Department of Cultural Heritage and Museology, Fudan University, Shanghai, China.,Institute of Archaeological Science, Fudan University, Shanghai, China
| |
Collapse
|
9
|
Hammond AS, Mavuso SS, Biernat M, Braun DR, Jinnah Z, Kuo S, Melaku S, Wemanya SN, Ndiema EK, Patterson DB, Uno KT, Palcu DV. New hominin remains and revised context from the earliest Homo erectus locality in East Turkana, Kenya. Nat Commun 2021; 12:1939. [PMID: 33850143 PMCID: PMC8044126 DOI: 10.1038/s41467-021-22208-x] [Citation(s) in RCA: 10] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/29/2020] [Accepted: 03/05/2021] [Indexed: 02/01/2023] Open
Abstract
The KNM-ER 2598 occipital is among the oldest fossils attributed to Homo erectus but questions have been raised about whether it may derive from a younger horizon. Here we report on efforts to relocate the KNM-ER 2598 locality and investigate its paleontological and geological context. Although located in a different East Turkana collection area (Area 13) than initially reported, the locality is stratigraphically positioned below the KBS Tuff and the outcrops show no evidence of deflation of a younger unit, supporting an age of >1.855 Ma. Newly recovered faunal material consists primarily of C4 grazers, further confirmed by enamel isotope data. A hominin proximal 3rd metatarsal and partial ilium were discovered <50 m from the reconstructed location where KNM-ER 2598 was originally found but these cannot be associated directly with the occipital. The postcrania are consistent with fossil Homo and may represent the earliest postcrania attributable to Homo erectus.
Collapse
Affiliation(s)
- Ashley S Hammond
- Division of Anthropology, American Museum of Natural History, New York, NY, USA.
- New York Consortium of Evolutionary Primatology (NYCEP), New York, NY, USA.
| | | | - Maryse Biernat
- School of Human Evolution and Social Change, Arizona State University, Tempe, AZ, USA
| | - David R Braun
- Department of Anthropology and Center for Advanced Study of Human Paleobiology, The George Washington University, Washington, DC, USA
- Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany
| | - Zubair Jinnah
- School of Geosciences, University of the Witwatersrand, Johannesburg, South Africa
| | - Sharon Kuo
- Department of Anthropology, Pennsylvania State University, University Park, PA, USA
| | - Sahleselasie Melaku
- Authority for Research and Conservation of Cultural Heritage (ARCCH), National Museum of Ethiopia, Addis Ababa, Ethiopia
- Paleoanthropology and Paleoenvironment Program, Addis Ababa University, Addis Ababa, Ethiopia
| | - Sylvia N Wemanya
- Archaeology Section, Department of Earth Sciences, National Museums of Kenya, Nairobi, Kenya
- Department of Archaeology and History, University of Nairobi, Nairobi, Kenya
| | - Emmanuel K Ndiema
- Archaeology Section, Department of Earth Sciences, National Museums of Kenya, Nairobi, Kenya
| | - David B Patterson
- Department of Biology, University of North Georgia, Dahlonega, GA, USA
| | - Kevin T Uno
- Division of Biology and Paleo Environment, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - Dan V Palcu
- Paleomagnetic Laboratory 'Fort Hoofddijk', Utrecht University, Utrecht, Netherlands
- Instituto Oceanográfico, Universidade de São Paulo, São Paulo, Brazil
| |
Collapse
|
10
|
Quinn RL, Lepre CJ. Contracting eastern African C 4 grasslands during the extinction of Paranthropus boisei. Sci Rep 2021; 11:7164. [PMID: 33785831 PMCID: PMC8009881 DOI: 10.1038/s41598-021-86642-z] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/04/2020] [Accepted: 03/18/2021] [Indexed: 02/01/2023] Open
Abstract
The extinction of the Paranthropus boisei estimated to just before 1 Ma occurred when C4 grasslands dominated landscapes of the Eastern African Rift System (EARS). P. boisei has been characterized as an herbivorous C4 specialist, and paradoxically, its demise coincided with habitats favorable to its dietary ecology. Here we report new pedogenic carbonate stable carbon (δ13CPC) and oxygen (δ18OPC) values (nodules = 53, analyses = 95) from an under-sampled interval (1.4-0.7 Ma) in the Turkana Basin (Kenya), one of the most fossiliferous locales of P. boisei. We combined our new results with published δ13CPC values from the EARS dated to 3-0 Ma, conducted time-series analysis of woody cover (ƒWC), and compared the EARS ƒWC trends to regional and global paleo-environmental and -climatic datasets. Our results demonstrate that the long-term rise of C4 grasslands was punctuated by a transient but significant increase in C3 vegetation and warmer temperatures, coincident with the Mid-Pleistocene Transition (1.3-0.7 Ma) and implicating a short-term rise in pCO2. The contraction of C4 grasslands escalated dietary competition amongst the abundant C4-feeders, likely influencing P. boisei's demise.
Collapse
Affiliation(s)
- Rhonda L. Quinn
- grid.263379.a0000 0001 2172 0072Department of Sociology, Anthropology, Social Work and Criminal Justice, Seton Hall University, 400 South Orange Ave, South Orange, NJ 07079 USA ,grid.430387.b0000 0004 1936 8796Department of Earth and Planetary Sciences, Rutgers University, 610 Taylor Road, Piscataway, NJ 08854 USA
| | - Christopher J. Lepre
- grid.430387.b0000 0004 1936 8796Department of Earth and Planetary Sciences, Rutgers University, 610 Taylor Road, Piscataway, NJ 08854 USA
| |
Collapse
|
11
|
Elton S, Dunn J. Baboon biogeography, divergence, and evolution: Morphological and paleoecological perspectives. J Hum Evol 2020; 145:102799. [DOI: 10.1016/j.jhevol.2020.102799] [Citation(s) in RCA: 9] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/11/2019] [Revised: 04/01/2020] [Accepted: 04/01/2020] [Indexed: 11/30/2022]
|
12
|
Abstract
Diet is a major driver of hominin evolution, but most of the geochemical evidence relies on carbon isotopes (δ13C). Here, we report enamel stable calcium isotope (δ44/42Ca) values against δ13C values for several hominins and co-existing primates in the Turkana Basin area, circa 4 to 2 Ma. Australopithecus anamensis clusters with mammal browsers, Kenyanthropus platyops is distinct from A. anamensis in foraging into more open environments and the coexisting Theropithecus brumpti encompasses both the grazer and omnivore/carnivore domains. Early Homo is remarkable for its wide distribution in δ44/42Ca values, possibly reflecting omnivorous and opportunistic preferences. Paranthropus boisei is uniquely distributed in the δ13C versus δ44/42Ca iso-space being distinct from all other hominins from the Turkana Basin area as well as from the co-existing Theropithecus oswaldi. Several hypotheses are explored to discuss the unique δ44/42Ca values of Paranthropus boisei including significant differences observed with δ44/42Ca values recently reported for P. robustus from South Africa, questioning the monophyly of this genus. Non-traditional stable isotopes, such as of calcium, have potential to expand our understanding of ancient diets. Here, Martin et al. use stable calcium isotopes recovered from fossil tooth enamel to compare the dietary ecology of hominins and other primates in the Turkana Basin 2-4 million years ago.
Collapse
|
13
|
Martínez LM, Estebaranz-Sánchez F, Ferràndez-Cañadell C, Romero A, Ribot F, Galbany J, Gibert L, Pérez-Pérez A. Buccal dental-microwear and feeding ecology of Early Pleistocene Theropithecus oswaldi from Cueva Victoria (Spain). J Hum Evol 2020; 142:102736. [PMID: 32193025 DOI: 10.1016/j.jhevol.2019.102736] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/13/2018] [Revised: 11/11/2019] [Accepted: 11/20/2019] [Indexed: 11/25/2022]
Abstract
Despite the scarcity of fossil specimens of Theropithecus oswaldi in Eurasia, its presence out of Africa attests to the great dispersal of this Papionini genus during the Early Pleistocene. In the present study, we analyze the buccal dental microwear of T. oswaldi (T. o. leakeyi) fossil specimens from Cueva Victoria (Southeastern Spain). This analysis is the first characterization of the feeding ecology of T. oswaldi in Europe. The buccal microwear pattern of the molar and premolar teeth of T. oswaldi from Cueva Victoria shows great similarities to that observed for the extant frugivorous forest-dwelling Mandrillus sphinx and mangabeys (Cercocebus sp.)-both species adapted to durophagous dietary habits-while significantly different from that observed for the gramnivorous Theropithecus gelada. These results suggest that T. oswaldi from Cueva Victoria could have exploited both hard-shelled fruits or seeds and succulent fruits from open and forested Mediterranean ecosystems.
Collapse
Affiliation(s)
- L M Martínez
- Departament de Biologia Evolutiva, Ecologia i Ciències Ambientals, Secció de Zoologia i Antropologia Biològica, Universitat de Barcelona, Av. Diagonal 643, 08014, Barcelona, Spain.
| | - F Estebaranz-Sánchez
- Departament de Biologia Evolutiva, Ecologia i Ciències Ambientals, Secció de Zoologia i Antropologia Biològica, Universitat de Barcelona, Av. Diagonal 643, 08014, Barcelona, Spain; Departament de Biologia Animal, Biologia Vegetal i Ecologia, Unitat d'Antropologia Biològica, Universitat Autònoma de Barcelona, Campus de Bellaterra, 08193, Bellaterra - Cerdanyola del Vallès, Spain
| | - C Ferràndez-Cañadell
- Departament Dinàmica de la Terra i de l'Oceà, Facultat de Ciències de la Terra, Universitat de Barcelona, Martí Franquès s/n, 08028, Barcelona, Spain
| | - A Romero
- Departamento de Biotecnología, Facultad de Ciencias, Universidad de Alicante, 99, 03080, Alicante, Spain
| | - F Ribot
- Museo Municipal de Prehistoria y Paleontología, Calle Las Tiendas s/n, 18858, Orce, Granada, Spain
| | - J Galbany
- Departament de Psicologia Clínica i Psicobiologia, Universitat de Barcelona, Facultat de Psicologia, Passeig de la Vall d'Hebron, 171, 08035, Barcelona, Spain; Center for the Advanced Study of Human Paleobiology, Department of Anthropology, The George Washington University, Washington DC, USA
| | - L Gibert
- Departament de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Universitat de Barcelona, Martí Franquès s/n, 08028, Barcelona, Spain
| | - A Pérez-Pérez
- Departament de Biologia Evolutiva, Ecologia i Ciències Ambientals, Secció de Zoologia i Antropologia Biològica, Universitat de Barcelona, Av. Diagonal 643, 08014, Barcelona, Spain
| |
Collapse
|
14
|
Diets of mammalian fossil fauna from Kanapoi, northwestern Kenya. J Hum Evol 2020; 140:102338. [DOI: 10.1016/j.jhevol.2017.05.005] [Citation(s) in RCA: 8] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/02/2016] [Revised: 04/27/2017] [Accepted: 05/04/2017] [Indexed: 11/19/2022]
|
15
|
Lin B, Foxfoot IR, Miller CM, Venkatamaran VV, Kerby JT, Bechtold EK, Kellogg BS, Nguyen N, Fashing PJ. Leopard predation on gelada monkeys at Guassa, Ethiopia. Am J Primatol 2020; 82:e23098. [PMID: 31994756 DOI: 10.1002/ajp.23098] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/17/2019] [Revised: 10/24/2019] [Accepted: 12/20/2019] [Indexed: 10/25/2022]
Abstract
Predation is widely believed to exert strong selective pressure on primate behavior and ecology but is difficult to study and rarely observed. In this study, we describe seven encounters between lone wild leopards (Panthera pardus) and herds of geladas (Theropithecus gelada) over a 6-year period in an intact Afroalpine grassland ecosystem at the Guassa Community Conservation Area, Ethiopia. Three encounters consisted of attempted predation on geladas by leopards, one of which was successful. All three attacks occurred in low-visibility microhabitats (dominated by tussock graminoids, mima mounds, or tall shrubs) that provided leopards with hidden viewsheds from which to ambush geladas. An additional four encounters did not result in an attempted attack but still document the consistently fearful responses of geladas to leopards. In encounters with leopards, geladas typically gave alarm calls (n = 7 of 7 encounters), reduced interindividual distances (n = 5), and collectively fled towards or remained at their sleeping cliffs (n = 7), the only significant refugia in the open-country habitat at Guassa. Geladas did not engage in mobbing behavior towards leopards. Encounters with leopards tended to occur on days when gelada herd sizes were small, raising the possibility that leopards, as ambush hunters, might stalk geladas on days when fewer eyes and ears make them less likely to be detected. We compare the behavioral responses of geladas to leopards at Guassa with those previously reported at Arsi and the Simien Mountains and discuss how gelada vulnerability and responses to leopards compare with those of other primate species living in habitats containing more refugia. Lastly, we briefly consider how living in multilevel societies may represent an adaptive response by geladas and other open-country primates to predation pressure from leopards and other large carnivores.
Collapse
Affiliation(s)
- Bing Lin
- Woodrow Wilson School of Public & International Affairs, Princeton University, Princeton, New Jersey
| | | | - Carrie M Miller
- Department of Anthropology, University of Minnesota, Minneapolis, Minnesota
| | | | - Jeffrey T Kerby
- Neukom Institute for Computational Science, Dartmouth College, Hanover, New Hampshire
| | - Emily K Bechtold
- Department of Microbiology, University of Massachusetts Amherst, Amherst, Massachusetts
| | - Bryce S Kellogg
- Forest Restoration Program, The Nature Conservancy, Bend, Oregon
| | - Nga Nguyen
- Department of Anthropology and Environmental Studies Program, California State University Fullerton, Fullerton, California
- Centre for Ecological and Evolutionary Synthesis (CEES), Department of Biosciences, University of Oslo, Oslo, Norway
| | - Peter J Fashing
- Department of Anthropology and Environmental Studies Program, California State University Fullerton, Fullerton, California
- Centre for Ecological and Evolutionary Synthesis (CEES), Department of Biosciences, University of Oslo, Oslo, Norway
| |
Collapse
|
16
|
Frost SR, Ward CV, Manthi FK, Plavcan JM. Cercopithecid fossils from Kanapoi, West Turkana, Kenya (2007-2015). J Hum Evol 2020; 140:102642. [PMID: 31959361 DOI: 10.1016/j.jhevol.2019.102642] [Citation(s) in RCA: 8] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/10/2017] [Revised: 06/27/2019] [Accepted: 07/12/2019] [Indexed: 11/26/2022]
Abstract
Recent fieldwork at Kanapoi has expanded the sample of fossil cercopithecids, facilitating a re-appraisal of their taxonomy. The assemblage now includes at least one species of cercopithecin, two papionins, and two colobines. The guenon Nanopithecus browni is similar in dental size to extant Miopithecus. We tentatively re-affirm the identification of Parapapio cf. ado and confirm the presence of Theropithecus. The colobines include a small form tentatively attributed to Kuseracolobus and a second larger species. The Kanapoi fossils represent the oldest occurrences of guenons in Africa and of the important genus Theropithecus, the most abundant and widespread primate in the Neogene of Africa. In the assemblage, Parapapio cf. ado is the most abundant form, comprising the majority of specimens. All of the other taxa are comparatively rare. Colobines make up a small part of the Kanapoi fossil assemblage compared to most other contemporary sites, including Allia Bay, Kenya, where, like Kanapoi, Australopithecus anamensis has been found. The presence of Theropithecus is consistent with the presence of some relatively open habitat at Kanapoi. While the ecological preferences of the small cercopithecin are unknown, most guenons are associated with relatively wooded habitats, as are most colobines, suggesting the availability of at least some wooded areas.
Collapse
Affiliation(s)
- Stephen R Frost
- Department of Anthropology, 1218 University of Oregon, Eugene, OR 97403-1218, USA.
| | - Carol V Ward
- Department of Pathology and Anatomical Sciences, M263 Medical Sciences Building, University of Missouri, Columbia, MO 65212, USA.
| | - Fredrick K Manthi
- Department of Earth Sciences, National Museums of Kenya, P.O. Box 40658, Nairobi, Kenya.
| | - J Michael Plavcan
- Department of Anthropology, 330 Old Main, University of Arkansas, Fayetteville, AR 72701, USA
| |
Collapse
|
17
|
The ecology of Australopithecus anamensis in the early Pliocene of Kanapoi, Kenya. J Hum Evol 2020; 140:102717. [PMID: 31916996 DOI: 10.1016/j.jhevol.2019.102717] [Citation(s) in RCA: 16] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/15/2019] [Revised: 10/09/2019] [Accepted: 10/14/2019] [Indexed: 11/24/2022]
Abstract
Australopithecus anamensis is a pivotal species in human evolution. It is likely to be the direct ancestor of Australopithecus afarensis and the species that may have given rise to the Homo and Paranthropus lineages. It had a suite of adaptations for habitual bipedalism and a diet that differed from that of earlier hominin species. Under what environmental and ecological conditions did this suite of adaptations arise? The early Pliocene site of Kanapoi in the Lake Turkana Basin of Kenya has the largest sample of A. anamensis in eastern Africa and a rich record of fossil vertebrates. Most Kanapoi fossils are chronologically well constrained by radiometrically dated tephras between the ages of 4.2 and 4.1 million years ago. Sedimentological, isotopic, and faunal data indicate that the environments of Kanapoi during the early Pliocene had a complex range of vegetation types that included closed woodlands, shrubs, and grasslands near a river (for most of the sequence) or lake. These were dynamic landscapes that could shift rapidly from fluvial to lacustrine conditions, and then back. Australopithecus anamensis shared its environments with at least 10 species of very large herbivores, which undoubtedly played a major role in modifying the landscape by opening wooded areas and providing pathways for bipedal hominins. Hominins may have competed for terrestrial resources with abundant suids (Nyanzachoerus and Notochoerus) and for arboreal resources with monkeys (Parapapio being the most common cercopithecid). Kanapoi had a formidable group of predators that included a very abundant species of hyena (Parahyaena howelli), two sabre-tooth felids (Dinofelis and Homotherium), a giant otter (Enhydriodon cf. dikikae), and three species of crocodiles. Various measures of abundance indicate that A. anamensis was an important component of the Kanapoi early Pliocene ecosystems, and that its key adaptations allowed this species to thrive in complex and dynamic landscapes.
Collapse
|
18
|
Martin F, Plastiras CA, Merceron G, Souron A, Boisserie JR. Dietary niches of terrestrial cercopithecines from the Plio-Pleistocene Shungura Formation, Ethiopia: evidence from Dental Microwear Texture Analysis. Sci Rep 2018; 8:14052. [PMID: 30232366 PMCID: PMC6145942 DOI: 10.1038/s41598-018-32092-z] [Citation(s) in RCA: 8] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/15/2018] [Accepted: 08/28/2018] [Indexed: 12/03/2022] Open
Abstract
This study aims to explore the feeding ecology of two terrestrial papionins, Papio and Theropithecus from the Shungura Formation in Ethiopia, the most complete stratigraphic and paleontological record of the African Plio-Pleistocene. Two aspects were evaluated using Dental Microwear Texture Analysis: differences in diet between the extinct genera and their extant relatives, and any potential dietary fluctuations over time. Amongst more than 2,500 cercopithecid dental remains, 154 Theropithecus molars and 60 Papio molars were considered. Thirty-nine extant wild baboons and 20 wild geladas were also considered. The results show that diets of extinct monkeys from Member G already differed between genera as it is the case for their extant representatives. The shearing facets on the Theropithecus molars display significant variations in microwear textures, suggesting several dietary shifts over time. Two events point to higher intakes of herbaceous monocots (tougher than dicots foliages), at about 2.91 Ma (between members B and C) and at 2.32 Ma (between members E and F). These two events are separated by an inverse trend at about 2.53 Ma (between members C and D). Some of these variations, such as between members E and F are supported by the enamel carbon isotopic composition of herbivorous mammals and with paleovegetation evidence.
Collapse
Affiliation(s)
- Florian Martin
- Laboratory Paleontology Evolution Paleoecosystems Paleoprimatology (PALEVOPRIM) - UMR CNRS-INEE/University of Poitiers, 86073, POITIERS CEDEX 9, France
| | | | - Gildas Merceron
- Laboratory Paleontology Evolution Paleoecosystems Paleoprimatology (PALEVOPRIM) - UMR CNRS-INEE/University of Poitiers, 86073, POITIERS CEDEX 9, France.
| | - Antoine Souron
- De la Préhistoire à l'Actuel: Culture, Environnement et Anthropologie (PACEA) - UMR 5199 CNRS/Université de Bordeaux/Ministère de la Culture et de la Communication, 33615, PESSAC CEDEX, France
| | - Jean-Renaud Boisserie
- Laboratory Paleontology Evolution Paleoecosystems Paleoprimatology (PALEVOPRIM) - UMR CNRS-INEE/University of Poitiers, 86073, POITIERS CEDEX 9, France.,Centre Français des Etudes Ethiopiennes (CFEE) - USR 3137 CNRS/Ministère de l'Europe et des Affaires Etrangères, Ambassade de France en Ethiopie, ADDIS ABABA, Ethiopia
| |
Collapse
|
19
|
Uno KT, Rivals F, Bibi F, Pante M, Njau J, de la Torre I. Large mammal diets and paleoecology across the Oldowan–Acheulean transition at Olduvai Gorge, Tanzania from stable isotope and tooth wear analyses. J Hum Evol 2018; 120:76-91. [DOI: 10.1016/j.jhevol.2018.01.002] [Citation(s) in RCA: 27] [Impact Index Per Article: 4.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/06/2017] [Revised: 12/27/2017] [Accepted: 01/02/2018] [Indexed: 11/27/2022]
|
20
|
Souron A. Morphology, diet, and stable carbon isotopes: On the diet of Theropithecus
and some limits of uniformitarianism in paleoecology. AMERICAN JOURNAL OF PHYSICAL ANTHROPOLOGY 2018; 166:261-267. [DOI: 10.1002/ajpa.23414] [Citation(s) in RCA: 10] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/07/2017] [Revised: 01/03/2018] [Accepted: 01/05/2018] [Indexed: 11/08/2022]
Affiliation(s)
- Antoine Souron
- PACEA, UMR 5199, Université de Bordeaux, Bâtiment B18, Allée Geoffroy Saint Hilaire, CS 50023; Pessac, 33615 France
- Human Evolution Research Center, University of California; Berkeley California 94720-3140
| |
Collapse
|
21
|
Landscape scale heterogeneity in the East Turkana ecosystem during the Okote Member (1.56–1.38 Ma). J Hum Evol 2017; 112:148-161. [PMID: 28760580 DOI: 10.1016/j.jhevol.2017.06.007] [Citation(s) in RCA: 19] [Impact Index Per Article: 2.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/31/2016] [Revised: 06/21/2017] [Accepted: 06/24/2017] [Indexed: 11/22/2022]
|
22
|
Frost SR, Saanane C, Starkovich BM, Schwartz H, Schrenk F, Harvati K. New cranium of the large cercopithecid primate Theropithecus oswaldi leakeyi (Hopwood, 1934) from the paleoanthropological site of Makuyuni, Tanzania. J Hum Evol 2017; 109:46-56. [PMID: 28688459 DOI: 10.1016/j.jhevol.2017.05.007] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/28/2016] [Revised: 05/08/2017] [Accepted: 05/11/2017] [Indexed: 11/30/2022]
Abstract
The Pleistocene hominin site of Makuyuni, near Lake Manyara, Tanzania, is known for fossils attributable to Homo and Acheulean artifacts (Ring et al., 2005; Kaiser et al., 2010; Frost et al., 2012). Here we describe the fossil primate material from the Manyara Beds, which includes the first nearly complete female cranium of Theropithecus oswaldi leakeyi and a proximal tibia from the same taxon. The cranium is dated to between 633 and 780 Ka and the tibia to the Pleistocene. The T. oswaldi lineage is one of the most important among Neogene mammals of Africa: it is both widespread and abundant. The size of the dentition, cranium, and tibia all confirm the previously recognized trend of increasing body size in this lineage and make their taxonomic assignments secure. The morphology of this specimen provides new insights into the evolution of this lineage through time, as well as its geographic variation and sexual dimorphism. The cranium also shows damage consistent with a mammalian carnivore, most likely a felid. The identification of this material as representing T. o. leakeyi agrees with the Middle Pleistocene age estimates for the MK4 locality in particular and the Manyara Beds in general.
Collapse
Affiliation(s)
- Stephen R Frost
- Department of Anthropology, University of Oregon, Eugene, OR 97403-1218, USA.
| | - Charles Saanane
- Department of Archeology and Heritage Studies, School of Humanities, University of Dar es Salaam, P.O. Box 35050, Tanzania
| | - Britt M Starkovich
- Senckenberg Centre for Human Evolution and Palaeoenvironment at Tübingen, and Institute for Archaeological Sciences, Eberhard Karls Universität Tübingen, 72070 Tübingen, Germany; School of Anthropology, University of Arizona, Tucson, AZ 85721, USA
| | - Hilde Schwartz
- Earth and Planetary Sciences, University of California, Santa Cruz, CA 95064, USA
| | | | - Katerina Harvati
- Paleoanthropology, Department of Geosciences, and Senckenberg Centre for Human Evolution and Palaeoenvironment, Eberhard Karls Universität Tübingen, 72070 Tübingen, Germany
| |
Collapse
|
23
|
Robinson JR, Rowan J, Campisano CJ, Wynn JG, Reed KE. Late Pliocene environmental change during the transition from Australopithecus to Homo. Nat Ecol Evol 2017; 1:159. [DOI: 10.1038/s41559-017-0159] [Citation(s) in RCA: 29] [Impact Index Per Article: 4.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/06/2016] [Accepted: 04/07/2017] [Indexed: 11/09/2022]
|
24
|
Sage RF. A portrait of the C4 photosynthetic family on the 50th anniversary of its discovery: species number, evolutionary lineages, and Hall of Fame. JOURNAL OF EXPERIMENTAL BOTANY 2017; 68:4039-4056. [PMID: 28110278 DOI: 10.1093/jxb/erx005] [Citation(s) in RCA: 19] [Impact Index Per Article: 2.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/20/2023]
Abstract
Fifty years ago, the C4 photosynthetic pathway was first characterized. In the subsequent five decades, much has been learned about C4 plants, such that it is now possible to place nearly all C4 species into their respective evolutionary lineages. Sixty-one independent lineages of C4 photosynthesis are identified, with additional, ancillary C4 origins possible in 12 of these principal lineages. The lineages produced ~8100 C4 species (5044 grasses, 1322 sedges, and 1777 eudicots). Using midpoints of stem and crown node dates in their respective phylogenies, the oldest and most speciose C4 lineage is the grass lineage Chloridoideae, estimated to be near 30 million years old. Most C4 lineages are estimated to be younger than 15 million years. Older C4 lineages tend to be more speciose, while those younger than 7 million years have <43 species each. To further highlight C4 photosynthesis for a 50th anniversary snapshot, a Hall of Fame comprised of the 40 most significant C4 species is presented. Over the next 50 years, preservation of the Earth's C4 diversity is a concern, largely because of habitat loss due to elevated CO2 effects, invasive species, and expanded agricultural activities. Ironically, some members of the C4 Hall of Fame are leading threats to the natural C4 flora due to their association with human activities on landscapes where most C4 plants occur.
Collapse
Affiliation(s)
- Rowan F Sage
- Department of Ecology and Evolutionary Biology, University of Toronto, 25 Willcocks Street, Toronto, ON M5R3C6
| |
Collapse
|
25
|
Martínez LM, Estebaranz-Sánchez F, Galbany J, Pérez-Pérez A. Testing Dietary Hypotheses of East African Hominines Using Buccal Dental Microwear Data. PLoS One 2016; 11:e0165447. [PMID: 27851745 PMCID: PMC5112956 DOI: 10.1371/journal.pone.0165447] [Citation(s) in RCA: 16] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/01/2016] [Accepted: 10/12/2016] [Indexed: 12/02/2022] Open
Abstract
There is much debate on the dietary adaptations of the robust hominin lineages during the Pliocene-Pleistocene transition. It has been argued that the shift from C3 to C4 ecosystems in Africa was the main factor responsible for the robust dental and facial anatomical adaptations of Paranthropus taxa, which might be indicative of the consumption of fibrous, abrasive plant foods in open environments. However, occlusal dental microwear data fail to provide evidence of such dietary adaptations and are not consistent with isotopic evidence that supports greater C4 food intake for the robust clades than for the gracile australopithecines. We provide evidence from buccal dental microwear data that supports softer dietary habits than expected for P. aethiopicus and P. boisei based both on masticatory apomorphies and isotopic analyses. On one hand, striation densities on the buccal enamel surfaces of paranthropines teeth are low, resembling those of H. habilis and clearly differing from those observed on H. ergaster, which display higher scratch densities indicative of the consumption of a wide assortment of highly abrasive foodstuffs. Buccal dental microwear patterns are consistent with those previously described for occlusal enamel surfaces, suggesting that Paranthropus consumed much softer diets than previously presumed and thus calling into question a strict interpretation of isotopic evidence. On the other hand, the significantly high buccal scratch densities observed in the H. ergaster specimens are not consistent with a highly specialized, mostly carnivorous diet; instead, they support the consumption of a wide range of highly abrasive food items.
Collapse
Affiliation(s)
- Laura Mónica Martínez
- Secció de Zoologia i Antropologia, Departament de Biologia Evolutiva, Ecologia i Ciències Ambientals, Facultat de Biologia, Universitat de Barcelona, Barcelona, Spain
| | - Ferran Estebaranz-Sánchez
- Secció de Zoologia i Antropologia, Departament de Biologia Evolutiva, Ecologia i Ciències Ambientals, Facultat de Biologia, Universitat de Barcelona, Barcelona, Spain
| | - Jordi Galbany
- Center for the Advanced Study of Human Paleobiology, Department of Anthropology, The George Washington University, Washington DC, United States of America
| | - Alejandro Pérez-Pérez
- Secció de Zoologia i Antropologia, Departament de Biologia Evolutiva, Ecologia i Ciències Ambientals, Facultat de Biologia, Universitat de Barcelona, Barcelona, Spain
| |
Collapse
|
26
|
Jolly CJ. A Life in Evolutionary Anthropology. ANNUAL REVIEW OF ANTHROPOLOGY 2016. [DOI: 10.1146/annurev-anthro-102215-095835] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Abstract
I am delighted to contribute this career piece, although there are many other aged physical anthropologists who are more distinguished! I have tried to avoid duplicating another retrospective rumination ( Jolly 2009 ) while describing personal academic experiences over the past 60 years or so. This is not a CV; I have concentrated on my main research themes, omitting some academic byways, teaching, textbooks, and edited volumes. The account is punctuated with opinionated comments, mostly on physical anthropology, but sometimes, rashly, on other anthropological specialties. It begins early, because my professional interests have deep roots, and finishes with a speculation about the future of physical anthropology, and anthropology in general, in the coming genomic age.
Collapse
|
27
|
Dietary ecology of fossil Theropithecus: Inferences from dental microwear textures of extant geladas from ecologically diverse sites. J Hum Evol 2016; 99:1-9. [DOI: 10.1016/j.jhevol.2016.05.010] [Citation(s) in RCA: 25] [Impact Index Per Article: 3.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/12/2015] [Revised: 02/16/2016] [Accepted: 05/19/2016] [Indexed: 11/23/2022]
|
28
|
Sage RF, Sultmanis S. Why are there no C 4 forests? JOURNAL OF PLANT PHYSIOLOGY 2016; 203:55-68. [PMID: 27481816 DOI: 10.1016/j.jplph.2016.06.009] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/11/2016] [Revised: 06/13/2016] [Accepted: 06/15/2016] [Indexed: 05/22/2023]
Abstract
C4 photosynthesis is absent from the arborescent life form, with the exception of seven Hawaiian Euphorbia species and a few desert shrubs that become arborescent with age. As a consequence, wherever C3 trees can establish, their height advantage enables them to outcompete low stature C4 vegetation. Had C4 photosynthesis been able to evolve in an arborescent life form, forest cover (by C4 trees) could have been much more extensive than today, with significant consequences for the biosphere. Here, we address why there are so few C4 trees. Physiological explanations associated with low light performance of C4 photosynthesis are not supported, because C4 shade-tolerant species exhibit similar performance as shade-tolerant C3 species in terms of quantum yield, steady-state photosynthetic and use of sunflecks. Hence, hypothetical C4 trees could occur in the regeneration niche of forests. Constraints associated with the evolutionary history of the C4 lineages are more plausible. Most C4 species are grasses and sedges, which lack meristems needed for arborescence, while most C4 eudicots are highly specialized for harsh (arid, saline, hot) or disturbed habitats where arborescence may be maladapted. Most C4 eudicot clades are also young, and have not had sufficient time to radiate beyond the extreme environments where C4 evolution is favored. In the case of the Hawaiian Euphorbia species, they belong to one of the oldest and most diverse C4 lineages, which primed this group to evolve arborescence in a low-competition environment that appeared on the remote Hawaiian Islands.
Collapse
Affiliation(s)
- Rowan F Sage
- Department of Ecology and Evolutionary Biology, University of Toronto, 25 Willcocks Street, Toronto, ON M5S3B2, Canada.
| | - Stefanie Sultmanis
- Department of Ecology and Evolutionary Biology, University of Toronto, 25 Willcocks Street, Toronto, ON M5S3B2, Canada
| |
Collapse
|
29
|
Hippopotamus (H. amphibius) diet change indicates herbaceous plant encroachment following megaherbivore population collapse. Sci Rep 2016; 6:32807. [PMID: 27616433 PMCID: PMC5018729 DOI: 10.1038/srep32807] [Citation(s) in RCA: 8] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/18/2016] [Accepted: 08/15/2016] [Indexed: 11/08/2022] Open
Abstract
Megaherbivores (>1000 kg) are critical for ecosystem health and function, but face population collapse and extinction globally. The future of these megaherbivore-impoverished ecosystems is difficult to predict, though many studies have demonstrated increasing representation of C3 woody plants. These studies rely on direct observational data, however, and tools for assessing decadal-scale changes in African ecology without observation are lacking. We use isotopic records of historical common hippopotamus (Hippopotamus amphibius) canines to quantify herbaceous vegetation change in Queen Elizabeth National Park, Uganda following a period of civil unrest and poaching. This poaching event led to population collapse of two threatened African megaherbivore species: hippopotamus and African elephants (Loxodonta africana). Serial carbon isotope ratios (δ(13)C) in canine enamel from individuals that lived between 1960-2000 indicated substantial increases in C3 herbaceous plants in their diet (<20% C3 in the 1960s to 30-45% C3 in the 80s and 90s), supported by other observational and ecological data. These data indicate megaherbivore loss results in succession of both woody and herbaceous C3 vegetation and further reaching effects, such as decreased grazing capacity and herbivore biodiversity in the area. Given multiple lines of evidence, these individuals appear to accurately capture herbaceous vegetation change in Mweya.
Collapse
|
30
|
Sage RF. A portrait of the C4 photosynthetic family on the 50th anniversary of its discovery: species number, evolutionary lineages, and Hall of Fame. JOURNAL OF EXPERIMENTAL BOTANY 2016; 67:4039-56. [PMID: 27053721 DOI: 10.1093/jxb/erw156] [Citation(s) in RCA: 75] [Impact Index Per Article: 9.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/09/2023]
Abstract
Fifty years ago, the C4 photosynthetic pathway was first characterized. In the subsequent five decades, much has been learned about C4 plants, such that it is now possible to place nearly all C4 species into their respective evolutionary lineages. Sixty-one independent lineages of C4 photosynthesis are identified, with additional, ancillary C4 origins possible in 12 of these principal lineages. The lineages produced ~8100 C4 species (5044 grasses, 1322 sedges, and 1777 eudicots). Using midpoints of stem and crown node dates in their respective phylogenies, the oldest and most speciose C4 lineage is the grass lineage Chloridoideae, estimated to be near 30 million years old. Most C4 lineages are estimated to be younger than 15 million years. Older C4 lineages tend to be more speciose, while those younger than 7 million years have <43 species each. To further highlight C4 photosynthesis for a 50th anniversary snapshot, a Hall of Fame comprised of the 40 most significant C4 species is presented. Over the next 50 years, preservation of the Earth's C4 diversity is a concern, largely because of habitat loss due to elevated CO2 effects, invasive species, and expanded agricultural activities. Ironically, some members of the C4 Hall of Fame are leading threats to the natural C4 flora due to their association with human activities on landscapes where most C4 plants occur.
Collapse
Affiliation(s)
- Rowan F Sage
- Department of Ecology and Evolutionary Biology, University of Toronto, 25 Willcocks Street, Toronto, ON M5R3C6
| |
Collapse
|
31
|
Curran SC, Haile-Selassie Y. Paleoecological reconstruction of hominin-bearing middle Pliocene localities at Woranso-Mille, Ethiopia. J Hum Evol 2016; 96:97-112. [DOI: 10.1016/j.jhevol.2016.04.002] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/21/2014] [Revised: 04/14/2016] [Accepted: 04/16/2016] [Indexed: 10/21/2022]
|
32
|
Crowley BE, Reitsema LJ, Oelze VM, Sponheimer M. Advances in primate stable isotope ecology-Achievements and future prospects. Am J Primatol 2015; 78:995-1003. [PMID: 26683892 DOI: 10.1002/ajp.22510] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/31/2015] [Revised: 11/24/2015] [Accepted: 11/25/2015] [Indexed: 12/28/2022]
Abstract
Stable isotope biogeochemistry has been used to investigate foraging ecology in non-human primates for nearly 30 years. Whereas early studies focused on diet, more recently, isotopic analysis has been used to address a diversity of ecological questions ranging from niche partitioning to nutritional status to variability in life history traits. With this increasing array of applications, stable isotope analysis stands to make major contributions to our understanding of primate behavior and biology. Most notably, isotopic data provide novel insights into primate feeding behaviors that may not otherwise be detectable. This special issue brings together some of the recent advances in this relatively new field. In this introduction to the special issue, we review the state of isotopic applications in primatology and its origins and describe some developing methodological issues, including techniques for analyzing different tissue types, statistical approaches, and isotopic baselines. We then discuss the future directions we envision for the field of primate isotope ecology. Am. J. Primatol. 78:995-1003, 2016. © 2015 Wiley Periodicals, Inc.
Collapse
Affiliation(s)
- Brooke E Crowley
- Departments of Geology and Anthropology, University of Cincinnati, Cincinnati, Ohio.
| | | | - Vicky M Oelze
- Department of Primatology, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany
| | - Matt Sponheimer
- Department of Anthropology, University of Colorado, Boulder, Colorado
| |
Collapse
|
33
|
Dietary change among hominins and cercopithecids in Ethiopia during the early Pliocene. Proc Natl Acad Sci U S A 2015; 112:12304-9. [PMID: 26371308 DOI: 10.1073/pnas.1424982112] [Citation(s) in RCA: 56] [Impact Index Per Article: 6.2] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
The incorporation of C4 resources into hominin diet signifies increased dietary breadth within hominins and divergence from the dietary patterns of other great apes. Morphological evidence indicates that hominin diet became increasingly diverse by 4.2 million years ago but may not have included large proportions of C4 foods until 800 thousand years later, given the available isotopic evidence. Here we use carbon isotope data from early to mid Pliocene hominin and cercopithecid fossils from Woranso-Mille (central Afar, Ethiopia) to constrain the timing of this dietary change and its ecological context. We show that both hominins and some papionins expanded their diets to include C4 resources as early as 3.76 Ma. Among hominins, this dietary expansion postdates the major dentognathic morphological changes that distinguish Australopithecus from Ardipithecus, but it occurs amid a continuum of adaptations to diets of tougher, harder foods and to committed terrestrial bipedality. In contrast, carbon isotope data from cercopithecids indicate that C4-dominated diets of the earliest members of the Theropithecus oswaldi lineage preceded the dental specialization for grazing but occurred after they were fully terrestrial. The combined data indicate that the inclusion of C4 foods in hominin diet occurred as part of broader ecological changes in African primate communities.
Collapse
|
34
|
Quinn RL. Influence of Plio-Pleistocene basin hydrology on the Turkana hominin enamel carbonate δ(18)O values. J Hum Evol 2015; 86:13-31. [PMID: 26277306 DOI: 10.1016/j.jhevol.2015.06.004] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/23/2014] [Revised: 06/02/2015] [Accepted: 06/07/2015] [Indexed: 10/23/2022]
Abstract
Stable oxygen isotopes of hominin enamel carbonate (δ(18)OEC) provide a window into aspects of past drinking behavior and diet, body size, breastfeeding and weaning, mobility, and paleoclimate. It is tempting to compare all hominins across time and space in order to gauge species-level adaptations to changing environments and niche separation between those living sympatrically. Basinal, sub-basinal, and micro-environmental differences, however, may exert an influence on variation in enamel carbonate isotopic values that must be reconciled before hominin species across Africa can be meaningfully compared. Plio-Pleistocene Turkana hominin δ(18)OEC values show a considerable spread, potentially revealing many intrinsic and extrinsic contributing factors operating on different scales. In this study, I examine Turkana hominin δ(18)OEC values relative to identity (taxon, tooth type and number, body size of taxon), dietary (δ(13)C value, Turkana coeval and modern mammalian δ(18)OEC values), and contextual (time, depositional environment) information of each specimen and collection locality and discuss various potential influences. Turkana hominin δ(18)OEC values may primarily reflect differences in imbibed water sources (lake vs. river) as a function of evolving basin hydrology.
Collapse
Affiliation(s)
- Rhonda L Quinn
- Department of Sociology, Anthropology and Social Work, Seton Hall University, South Orange, NJ 07079, USA; Department of Earth and Planetary Sciences, Rutgers University, USA.
| |
Collapse
|
35
|
Abstract
Australopithecus bahrelghazali, its origin and palaeobiology are not well understood. Reported from only one location some several thousand kilometres away from East African Pliocene hominin sites, it appears to have predominantly fed on C4 sources. Yet, it lacks the morphological adaptations of other primate C4 consumers like Paranthropus boisei and Theropithecus oswaldi. Furthermore, although considered to belong to Australopithecus afarensis by most researchers, A. bahrelghazali appears to differ from the former in a key aspect of its morphology: enamel thickness. To assess the phylogeny and palaeobiology of A. bahrelghazali, I first evaluate the dietary adaptations and energetics of A. bahrelghazali using empirical data of the feeding ecology of extant baboons, Papio cynocephalus. Information published on A. bahrelghazali morphology and habitat preference is used to select C4 foods with the appropriate mechanical properties and availability within the environment to create the models. By altering the feeding time on various food categories, I then test whether A. bahrelghazali could have subsisted on a C4 diet, thus accounting for the δ(13)C composition of its dental tissue. The effects of body mass on the volume of food consumed are taken into account. The outcomes of these simulations indicate that A. bahrelghazali could have subsisted on a diet of predominantly sedges, albeit with limitations. At higher energy requirements, i.e., above 3.5 times the BMR, it would be difficult for a medium-sized primate to obtain sufficient energy from a sedge-based diet. This is apparently due to constraints on foraging/feeding time, not because of the nutritional value of sedges per se. These results are discussed against the backdrop of A. bahrelghazali biogeography, palaeoenvironment, and phylogeny. The combined evidence makes it plausible to suggest that Northern Chad may have been a refugium for migrating mammals, including hominins, and throws new light on the deep history of A. bahrelghazali.
Collapse
|
36
|
Schroer K, Wood B. The role of character displacement in the molarization of hominin mandibular premolars. Evolution 2015; 69:1630-1642. [PMID: 25913032 DOI: 10.1111/evo.12672] [Citation(s) in RCA: 7] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/24/2014] [Accepted: 04/21/2015] [Indexed: 11/24/2022]
Abstract
Closely related species are likely to experience resource competition in areas where their ranges overlap. Fossil evidence suggests that hominins in East Africa c. 2-1.5 million years ago may have lived synchronically and sympatrically, and that competition may have contributed to the different tooth sizes observed in Homo and Paranthropus. To assess the likelihood that these taxa overlapped, we applied a character displacement model to the postcanine tooth size of fossil hominins and validated this model in populations of living primates. Mandibular fourth premolar (P4 ) crown size was measured from fossil taxa and from living primate species where dietary overlap is established. Dimensions of the P4 crown were fitted to a character matrix and described as the response variables of a generalized linear model that took taxon and location as input variables. The model recovered significant divergence in samples of closely related, living primates. When applied to fossil hominins the same model detected strong indications of character displacement between early Homo and Paranthropus (P = 0.002) on the basis of their P4 crown size. Our study is an example of how ecologically informed morphologies measured in appropriate extant referents can provide a comparative context for assessing community and ecological evolution in the fossil record.
Collapse
Affiliation(s)
- Kes Schroer
- Neukom Institute for Computational Science, Dartmouth, 6047 Silsby Hall, Hanover, New Hampshire, 03755.,Department of Anthropology, Dartmouth, 6047 Silsby Hall, Hanover, New Hampshire, 03755
| | - Bernard Wood
- Center for the Advanced Study of Hominid Paleobiology, The George Washington University, 2110 G St NW, Washington, DC, 20052
| |
Collapse
|
37
|
Archaeogenomic insights into the adaptation of plants to the human environment: pushing plant-hominin co-evolution back to the Pliocene. J Hum Evol 2015; 79:150-7. [PMID: 25577019 DOI: 10.1016/j.jhevol.2014.10.014] [Citation(s) in RCA: 23] [Impact Index Per Article: 2.6] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/01/2014] [Revised: 07/25/2014] [Accepted: 10/31/2014] [Indexed: 01/05/2023]
Abstract
The colonization of the human environment by plants, and the consequent evolution of domesticated forms is increasingly being viewed as a co-evolutionary plant-human process that occurred over a long time period, with evidence for the co-evolutionary relationship between plants and humans reaching ever deeper into the hominin past. This developing view is characterized by a change in emphasis on the drivers of evolution in the case of plants. Rather than individual species being passive recipients of artificial selection pressures and ultimately becoming domesticates, entire plant communities adapted to the human environment. This evolutionary scenario leads to systems level genetic expectations from models that can be explored through ancient DNA and Next Generation Sequencing approaches. Emerging evidence suggests that domesticated genomes fit well with these expectations, with periods of stable complex evolution characterized by large amounts of change associated with relatively small selective value, punctuated by periods in which changes in one-half of the plant-hominin relationship cause rapid, low-complexity adaptation in the other. A corollary of a single plant-hominin co-evolutionary process is that clues about the initiation of the domestication process may well lie deep within the hominin lineage.
Collapse
|
38
|
Frost SR, Jablonski NG, Haile-Selassie Y. Early Pliocene Cercopithecidae from Woranso-Mille (Central Afar, Ethiopia) and the origins of the Theropithecus oswaldi lineage. J Hum Evol 2014; 76:39-53. [DOI: 10.1016/j.jhevol.2014.05.003] [Citation(s) in RCA: 50] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/20/2013] [Revised: 05/05/2014] [Accepted: 05/05/2014] [Indexed: 11/15/2022]
|
39
|
Fashing PJ, Nguyen N, Venkataraman VV, Kerby JT. Gelada feeding ecology in an intact ecosystem at Guassa, Ethiopia: Variability over time and implications for theropith and hominin dietary evolution. AMERICAN JOURNAL OF PHYSICAL ANTHROPOLOGY 2014; 155:1-16. [DOI: 10.1002/ajpa.22559] [Citation(s) in RCA: 63] [Impact Index Per Article: 6.3] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/17/2014] [Revised: 06/05/2014] [Accepted: 06/06/2014] [Indexed: 11/11/2022]
Affiliation(s)
- Peter J. Fashing
- Department of Anthropology; California State University Fullerton; 800 N. State College Boulevard Fullerton CA 92834
- Environmental Studies Program; California State University Fullerton; 800 N. State College Boulevard Fullerton CA 92834
| | - Nga Nguyen
- Department of Anthropology; California State University Fullerton; 800 N. State College Boulevard Fullerton CA 92834
- Environmental Studies Program; California State University Fullerton; 800 N. State College Boulevard Fullerton CA 92834
| | | | - Jeffrey T. Kerby
- The Polar Center and Department of Biology; Pennsylvania State University; University Park PA 16802
| |
Collapse
|
40
|
Patnaik R, Cerling TE, Uno KT, Fleagle JG. Diet and Habitat of Siwalik PrimatesIndopithecus, SivaladapisandTheropithecus. ANN ZOOL FENN 2014. [DOI: 10.5735/086.051.0214] [Citation(s) in RCA: 18] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/25/2022]
|
41
|
Macho GA. Baboon feeding ecology informs the dietary niche of Paranthropus boisei. PLoS One 2014; 9:e84942. [PMID: 24416315 PMCID: PMC3885648 DOI: 10.1371/journal.pone.0084942] [Citation(s) in RCA: 28] [Impact Index Per Article: 2.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/02/2013] [Accepted: 11/29/2013] [Indexed: 11/19/2022] Open
Abstract
Hominins are generally considered eclectic omnivores like baboons, but recent isotope studies call into question the generalist status of some hominins. Paranthropus boisei and Australopithecus bahrelghazali derived 75%-80% of their tissues' δ(13)C from C4 sources, i.e. mainly low-quality foods like grasses and sedges. Here I consider the energetics of P. boisei and the nutritional value of C4 foods, taking into account scaling issues between the volume of food consumed and body mass, and P. boisei's food preference as inferred from dento-cranial morphology. Underlying the models are empirical data for Papio cynocephalus dietary ecology. Paranthropus boisei only needed to spend some 37%-42% of its daily feeding time (conservative estimate) on C4 sources to meet 80% of its daily requirements of calories, and all its requirements for protein. The energetic requirements of 2-4 times the basal metabolic rate (BMR) common to mammals could therefore have been met within a 6-hour feeding/foraging day. The findings highlight the high nutritional yield of many C4 foods eaten by baboons (and presumably hominins), explain the evolutionary success of P. boisei, and indicate that P. boisei was probably a generalist like other hominins. The diet proposed is consistent with the species' derived morphology and unique microwear textures. Finally, the results highlight the importance of baboon/hominin hand in food acquisition and preparation.
Collapse
|
42
|
Sponheimer M, Alemseged Z, Cerling TE, Grine FE, Kimbel WH, Leakey MG, Lee-Thorp JA, Manthi FK, Reed KE, Wood BA, Wynn JG. Isotopic evidence of early hominin diets. Proc Natl Acad Sci U S A 2013; 110:10513-10518. [PMCID: PMC3696771 DOI: 10.1073/pnas.1222579110] [Citation(s) in RCA: 130] [Impact Index Per Article: 11.8] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/07/2023] Open
Abstract
Carbon isotope studies of early hominins from southern Africa showed that their diets differed markedly from the diets of extant apes. Only recently, however, has a major influx of isotopic data from eastern Africa allowed for broad taxonomic, temporal, and regional comparisons among hominins. Before 4 Ma, hominins had diets that were dominated by C3 resources and were, in that sense, similar to extant chimpanzees. By about 3.5 Ma, multiple hominin taxa began incorporating 13C-enriched [C4 or crassulacean acid metabolism (CAM)] foods in their diets and had highly variable carbon isotope compositions which are atypical for African mammals. By about 2.5 Ma, Paranthropus in eastern Africa diverged toward C4/CAM specialization and occupied an isotopic niche unknown in catarrhine primates, except in the fossil relations of grass-eating geladas (Theropithecus gelada ). At the same time, other taxa (e.g., Australopithecus africanus ) continued to have highly mixed and varied C3/C4 diets. Overall, there is a trend toward greater consumption of 13C-enriched foods in early hominins over time, although this trend varies by region. Hominin carbon isotope ratios also increase with postcanine tooth area and mandibular cross-sectional area, which could indicate that these foods played a role in the evolution of australopith masticatory robusticity. The 13C-enriched resources that hominins ate remain unknown and must await additional integration of existing paleodietary proxy data and new research on the distribution, abundance, nutrition, and mechanical properties of C4 (and CAM) plants.
Collapse
Affiliation(s)
- Matt Sponheimer
- Department of Anthropology, University of Colorado, Boulder, CO 80309
| | - Zeresenay Alemseged
- Department of Anthropology, California Academy of Sciences, San Francisco, CA 94118
| | - Thure E. Cerling
- Department of Geology and Geophysics, University of Utah, Salt Lake City, UT 84112
| | - Frederick E. Grine
- Department of Anthropology, Stony Brook University, Stony Brook, NY 11794
| | - William H. Kimbel
- Institute of Human Origins, School of Human Evolution and Social Change, Arizona State University, Tempe, AZ 85287
| | - Meave G. Leakey
- Department of Anthropology, Stony Brook University, Stony Brook, NY 11794
- Turkana Basin Institute, 00502 Nairobi, Kenya
| | - Julia A. Lee-Thorp
- Research Laboratory for Archaeology, Oxford University, Oxford OX1 3QY, United Kingdom
| | | | - Kaye E. Reed
- Institute of Human Origins, School of Human Evolution and Social Change, Arizona State University, Tempe, AZ 85287
| | - Bernard A. Wood
- Center for the Advanced Study of Hominid Paleobiology, Department of Anthropology, George Washington University, Washington, DC 20052; and
| | - Jonathan G. Wynn
- Department of Geology, University of South Florida, Tampa, FL 33620
| |
Collapse
|
43
|
|
44
|
Abstract
Hominin fossil evidence in the Turkana Basin in Kenya from ca. 4.1 to 1.4 Ma samples two archaic early hominin genera and records some of the early evolutionary history of Paranthropus and Homo. Stable carbon isotopes in fossil tooth enamel are used to estimate the fraction of diet derived from C3 or C4 resources in these hominin taxa. The earliest hominin species in the Turkana Basin, Australopithecus anamensis, derived nearly all of its diet from C3 resources. Subsequently, by ca. 3.3 Ma, the later Kenyanthropus platyops had a very wide dietary range--from virtually a purely C3 resource-based diet to one dominated by C4 resources. By ca. 2 Ma, hominins in the Turkana Basin had split into two distinct groups: specimens attributable to the genus Homo provide evidence for a diet with a ca. 65/35 ratio of C3- to C4-based resources, whereas P. boisei had a higher fraction of C4-based diet (ca. 25/75 ratio). Homo sp. increased the fraction of C4-based resources in the diet through ca. 1.5 Ma, whereas P. boisei maintained its high dependency on C4-derived resources.
Collapse
|