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Comans CM, Smart SM, Kast ER, Lu Y, Lüdecke T, Leichliter JN, Sigman DM, Ikejiri T, Martínez-García A. Enameloid-bound δ 15 N reveals large trophic separation among Late Cretaceous sharks in the northern Gulf of Mexico. Geobiology 2024; 22:e12585. [PMID: 38385603 DOI: 10.1111/gbi.12585] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/05/2023] [Revised: 11/21/2023] [Accepted: 01/03/2024] [Indexed: 02/23/2024]
Abstract
The nitrogen isotopic composition (15 N/14 N ratio, or δ15 N) of enameloid-bound organic matter (δ15 NEB ) in shark teeth was recently developed to investigate the biogeochemistry and trophic structures (i.e., food webs) of the ancient ocean. Using δ15 NEB , we present the first nitrogen isotopic evidence for trophic differences between shark taxa from a single fossil locality. We analyze the teeth of four taxa (Meristodonoides, Ptychodus, Scapanorhynchus, and Squalicorax) from the Late Cretaceous (83-84 Ma) Trussells Creek site in Alabama, USA, and compare the N isotopic findings with predictions from tooth morphology, the traditional method for inferring shark paleo-diets. Our δ15 NEB data indicate two distinct trophic groups, with averages separated by 6.1 ± 2.1‰. The lower group consists of Meristodonoides and Ptychodus, and the higher group consists of Scapanorhynchus and Squalicorax (i.e., lamniforms). This δ15 NEB difference indicates a 1.5 ± 0.5 trophic-level separation between the two groups, a finding that is in line with paleontological predictions of a higher trophic level for these lamniforms over Meristodonoides and Ptychodus. However, the δ15 NEB of Meristodonoides is lower than suggested by tooth morphology, although consistent with mechanical tests suggesting that higher trophic-level bony fishes were not a major component of their diet. Further, δ15 NEB indicates that the two sampled lamniform taxa fed at similar trophic levels despite their different inferred tooth functions. These two findings suggest that tooth morphology alone may not always be a sufficient indicator of dietary niche. The large trophic separation revealed by the δ15 NEB offset leaves open the possibility that higher trophic-level lamniforms, such as those measured here, preyed upon smaller, lower trophic-level sharks like Meristodonoides.
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Affiliation(s)
- Chelsea M Comans
- Department of Geological Sciences, The University of Alabama, Tuscaloosa, Alabama, USA
| | - Sandi M Smart
- Department of Geological Sciences, The University of Alabama, Tuscaloosa, Alabama, USA
- Max Plank Institute for Chemistry, Mainz, Germany
| | - Emma R Kast
- Department of Earth Sciences, University of Cambridge, Cambridge, UK
| | - YueHan Lu
- Department of Geological Sciences, The University of Alabama, Tuscaloosa, Alabama, USA
| | - Tina Lüdecke
- Max Plank Institute for Chemistry, Mainz, Germany
| | | | - Daniel M Sigman
- Department of Geosciences, Princeton University, Princeton, New Jersey, USA
| | - Takehito Ikejiri
- Department of Geological Sciences, The University of Alabama, Tuscaloosa, Alabama, USA
- Alabama Museum of Natural History, The University of Alabama, Tuscaloosa, Alabama, USA
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Kast ER, Griffiths ML, Kim SL, Rao ZC, Shimada K, Becker MA, Maisch HM, Eagle RA, Clarke CA, Neumann AN, Karnes ME, Lüdecke T, Leichliter JN, Martínez-García A, Akhtar AA, Wang XT, Haug GH, Sigman DM. Cenozoic megatooth sharks occupied extremely high trophic positions. Sci Adv 2022; 8:eabl6529. [PMID: 35731884 PMCID: PMC9217088 DOI: 10.1126/sciadv.abl6529] [Citation(s) in RCA: 9] [Impact Index Per Article: 4.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 07/29/2021] [Accepted: 05/05/2022] [Indexed: 06/15/2023]
Abstract
Trophic position is a fundamental characteristic of animals, yet it is unknown in many extinct species. In this study, we ground-truth the 15N/14N ratio of enameloid-bound organic matter (δ15NEB) as a trophic level proxy by comparison to dentin collagen δ15N and apply this method to the fossil record to reconstruct the trophic level of the megatooth sharks (genus Otodus). These sharks evolved in the Cenozoic, culminating in Otodus megalodon, a shark with a maximum body size of more than 15 m, which went extinct 3.5 million years ago. Very high δ15NEB values (22.9 ± 4.4‰) of O. megalodon from the Miocene and Pliocene show that it occupied a higher trophic level than is known for any marine species, extinct or extant. δ15NEB also indicates a dietary shift in sharks of the megatooth lineage as they evolved toward the gigantic O. megalodon, with the highest trophic level apparently reached earlier than peak size.
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Affiliation(s)
- Emma R. Kast
- Department of Geosciences, Princeton University, Princeton, NJ 08544, USA
- Department of Earth Sciences, University of Cambridge, Cambridge, CB23EQ, UK
| | - Michael L. Griffiths
- Department of Environmental Science, William Paterson University of New Jersey, Wayne, NJ 07470, USA
| | - Sora L. Kim
- Department of Life and Environmental Sciences, University of California Merced, Merced, CA 95343, USA
| | - Zixuan C. Rao
- Department of Geosciences, Princeton University, Princeton, NJ 08544, USA
| | - Kenshu Shimada
- Department of Environmental Science and Studies, DePaul University, Chicago, IL 60614, USA
- Department of Biological Sciences, DePaul University, Chicago, IL 60614, USA
- Sternberg Museum of Natural History, Fort Hays State University, Hays, KS 67601, USA
| | - Martin A. Becker
- Department of Environmental Science, William Paterson University of New Jersey, Wayne, NJ 07470, USA
| | - Harry M. Maisch
- Department of Marine and Earth Sciences, Florida Gulf Coast University, Fort Myers, FL 33965, USA
| | - Robert A. Eagle
- Department of Atmospheric and Oceanic Sciences. Institute of the Environment and Sustainability, University of California, Los Angeles, CA 90095, USA
| | - Chelesia A. Clarke
- Department of Environmental Science, William Paterson University of New Jersey, Wayne, NJ 07470, USA
| | - Allison N. Neumann
- Department of Environmental Science, William Paterson University of New Jersey, Wayne, NJ 07470, USA
| | - Molly E. Karnes
- Department of Life and Environmental Sciences, University of California Merced, Merced, CA 95343, USA
| | - Tina Lüdecke
- Emmy Noether Group for Hominin Meat Consumption, Max Planck Institute for Chemistry, 55128 Mainz, Germany
- Senckenberg Biodiversity and Climate Research Centre, 60325 Frankfurt, Germany
| | - Jennifer N. Leichliter
- Emmy Noether Group for Hominin Meat Consumption, Max Planck Institute for Chemistry, 55128 Mainz, Germany
- Johannes Gutenberg University, Institute of Geosciences, 55128 Mainz, Germany
| | - Alfredo Martínez-García
- Department of Climate Geochemistry, Max Planck Institute for Chemistry, 55128 Mainz, Germany
| | - Alliya A. Akhtar
- Department of Geosciences, Princeton University, Princeton, NJ 08544, USA
| | - Xingchen T. Wang
- Department of Earth and Environmental Sciences, Boston College, Chestnut Hill, MA 02467, USA
| | - Gerald H. Haug
- Department of Climate Geochemistry, Max Planck Institute for Chemistry, 55128 Mainz, Germany
- Department of Earth Sciences, ETH Zürich, CH-8092 Zürich, Switzerland
| | - Daniel M. Sigman
- Department of Geosciences, Princeton University, Princeton, NJ 08544, USA
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Kast ER, Stolper DA, Auderset A, Higgins JA, Ren H, Wang XT, Martínez-García A, Haug GH, Sigman DM. Nitrogen isotope evidence for expanded ocean suboxia in the early Cenozoic. Science 2019; 364:386-389. [PMID: 31023923 DOI: 10.1126/science.aau5784] [Citation(s) in RCA: 27] [Impact Index Per Article: 5.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/06/2018] [Accepted: 03/26/2019] [Indexed: 11/03/2022]
Abstract
The million-year variability of the marine nitrogen cycle is poorly understood. Before 57 million years (Ma) ago, the 15N/14N ratio (δ15N) of foraminifera shell-bound organic matter from three sediment cores was high, indicating expanded water column suboxia and denitrification. Between 57 and 50 Ma ago, δ15N declined by 13 to 16 per mil in the North Pacific and by 3 to 8 per mil in the Atlantic. The decline preceded global cooling and appears to have coincided with the early stages of the Asia-India collision. Warm, salty intermediate-depth water forming along the Tethys Sea margins may have caused the expanded suboxia, ending with the collision. From 50 to 35 Ma ago, δ15N was lower than modern values, suggesting widespread sedimentary denitrification on broad continental shelves. δ15N rose at 35 Ma ago, as ice sheets grew, sea level fell, and continental shelves narrowed.
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Affiliation(s)
- Emma R Kast
- Department of Geosciences, Princeton University, Princeton, NJ 08540, USA.
| | - Daniel A Stolper
- Department of Earth and Planetary Science, University of California, Berkeley, CA 94720, USA.,Earth and Environmental Sciences Area, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA
| | - Alexandra Auderset
- Department of Climate Geochemistry, Max Planck Institute for Chemistry, 55128 Mainz, Germany.,Department of Earth Sciences, ETH Zürich, CH-8092 Zürich, Switzerland
| | - John A Higgins
- Department of Geosciences, Princeton University, Princeton, NJ 08540, USA
| | - Haojia Ren
- Research Center for Future Earth, National Taiwan University, Taipei 106, Taiwan
| | - Xingchen T Wang
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA
| | - Alfredo Martínez-García
- Department of Climate Geochemistry, Max Planck Institute for Chemistry, 55128 Mainz, Germany
| | - Gerald H Haug
- Department of Climate Geochemistry, Max Planck Institute for Chemistry, 55128 Mainz, Germany.,Department of Earth Sciences, ETH Zürich, CH-8092 Zürich, Switzerland
| | - Daniel M Sigman
- Department of Geosciences, Princeton University, Princeton, NJ 08540, USA
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