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Ao D, Wang B, Wang Y, Chen Y, Anum R, Feng C, Ji M, Liang C, An S. Grassland degraded patchiness reduces microbial necromass content but increases contribution to soil organic carbon accumulation. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 951:175717. [PMID: 39197785 DOI: 10.1016/j.scitotenv.2024.175717] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/03/2024] [Revised: 08/20/2024] [Accepted: 08/21/2024] [Indexed: 09/01/2024]
Abstract
Plant and microbially derived carbon (C) are the two major sources of soil organic carbon (SOC), and their ratio impacts SOC composition, accumulation, stability, and turnover. The contributions of and the key factors defining the plant and microbial C in SOC with grassland patches are not well known. Here, we aim to address this issue by analyzing lignin phenols, amino sugars, glomalin-related soil proteins (GRSP), enzyme activities, particulate organic carbon (POC), and mineral-associated organic carbon (MAOC). Shrubby patches showed increased SOC and POC due to higher plant inputs, thereby stimulating plant-derived C (e.g., lignin phenol) accumulation. While degraded and exposed patches exhibited higher microbially derived C due to reduced plant input. After grassland degradation, POC content decreased faster than MAOC, and plant biomarkers (lignin phenols) declined faster than microbial biomarkers (amino sugars). As grassland degradation intensified, microbial necromass C and GRSP (gelling agents) increased their contribution to SOC formation. Grassland degradation stimulated the stabilization of microbially derived C in the form of MAOC. Further analyses revealed that microorganisms have a C and P co-limitation, stimulating the recycling of necromass, resulting in the proportion of microbial necromass C in the SOC remaining essentially stable with grassland degradation. Overall, with the grassland degradation, the relative proportion of the plant component decreases while than of the microbial component increases and existed in the form of MAOC. This is attributed to the physical protection of SOC by GRSP cementation. Therefore, different sources of SOC should be considered in evaluating SOC responses to grassland degradation, which has important implications for predicting dynamics in SOC under climate change and anthropogenic factors.
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Affiliation(s)
- Deng Ao
- College of Nature Resources and Environment, Northwest A&F University, Yangling 712100, China
| | - Baorong Wang
- College of Grassland Agriculture, Northwest A&F University, Yangling 712100, China
| | - Yubin Wang
- College of Nature Resources and Environment, Northwest A&F University, Yangling 712100, China
| | - Yuanjia Chen
- Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China
| | - Rafiq Anum
- Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China
| | - Chenglong Feng
- Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China
| | - Mukan Ji
- Center for Pan-third Pole Environment, Lanzhou University, Lanzhou 730000, China
| | - Chao Liang
- Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China
| | - Shaoshan An
- College of Nature Resources and Environment, Northwest A&F University, Yangling 712100, China; Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China; State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, China.
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2
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Vaidya S, Hoffmann M, Dubbert M, Kramp K, Schmidt M, Verch G, Sommer M, Augustin J. Topsoil dilution by subsoil admixture had less impact on soil organic carbon stock development than fertilizer form and erosion state. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 946:174243. [PMID: 38944309 DOI: 10.1016/j.scitotenv.2024.174243] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/06/2024] [Revised: 06/21/2024] [Accepted: 06/21/2024] [Indexed: 07/01/2024]
Abstract
Enhancing the agroecosystems carbon (C) sink function for climate mitigation faced challenges, particularly with traditional measures with limited suitability for increasing soil organic carbon (SOC) stocks. Inducing a SOC undersaturation in the topsoil by abrupt subsoil admixture is a way to create an additional C sink. However, the deep tillage traditionally used for this topsoil dilution was not always successful. It was due to a lack of knowledge and suitable approaches to record the effect of all relevant factors in SOC recovery, including soil conditions and fertilizer forms. We addressed these problems by establishing a three-factorial experiment: I) "moderate topsoil dilution," II) "N fertilization form," and III) "soil erosion state," representing three soil types in the hummocky ground moraine landscape of NE Germany. SOC dynamics were determined over a year of winter rye cropping using a novel robotic chamber system capable of measuring CO2 exchange on 36 experimental plots with a reduced methodological bias than previous measuring systems. The averaged net ecosystem carbon balance, a proxy for SOC stock change, indicated that topsoil dilution only reduced further SOC losses. The N fertilizer form had a significantly stronger and more differentiated effect. While the mineral N fertilization consistently produced only C sources, the organic fertilization, in combination with the diluted topsoil, led to a C sink. This C-sink function was, however, more pronounced in the eroded soil than in the non-eroded soil. Overall, the results have made clear that the impact of topsoil dilution on the further development of the SOC stock is only possible if the effect of other relevant factors, such as N fertilizer form and erosion state, are taken into account.
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Affiliation(s)
- Shrijana Vaidya
- Leibniz Center for Agricultural Landscape Research (ZALF), working group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany; Albrecht Daniel Thaer Institute, Faculty of Life Science, Humboldt-Universität zu Berlin, 14195 Berlin, Germany.
| | - Mathias Hoffmann
- Leibniz Center for Agricultural Landscape Research (ZALF), working group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
| | - Maren Dubbert
- Leibniz Center for Agricultural Landscape Research (ZALF), working group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
| | - Katja Kramp
- Leibniz Center for Agricultural Landscape Research (ZALF), working group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
| | - Marten Schmidt
- Leibniz Center for Agricultural Landscape Research (ZALF), working group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
| | - Gernot Verch
- Leibniz Center for Agricultural Landscape Research (ZALF), Experimental Infrastructure Platform, Steinfurther Straße 14, 17291 Prenzlau, Germany
| | - Michael Sommer
- Leibniz Center for Agricultural Landscape Research (ZALF), working group for Landscape Pedology, Eberswalder Str. 84, 15374 Müncheberg, Germany; University of Potsdam, Institute of Environmental Science and Geography, Karl-Liebknecht-Str.24-25, 14476 Potsdam, Germany
| | - Jürgen Augustin
- Leibniz Center for Agricultural Landscape Research (ZALF), working group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
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Cha J, Kim JH, Jung JY, Nam SI, Hong S. Chronological distribution and potential sources of persistent toxic substances in soils from the glacier foreland of Midtre Lovénbreen, Svalbard. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2024; 357:124387. [PMID: 38897275 DOI: 10.1016/j.envpol.2024.124387] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/08/2024] [Revised: 06/11/2024] [Accepted: 06/16/2024] [Indexed: 06/21/2024]
Abstract
Despite its reputation as one of the cleanest regions globally, recent studies have identified the presence of various persistent toxic substances (PTSs) in the environmental matrices collected from Svalbard. This study investigated the chronological distribution and potential sources of 81 PTSs in soils from the glacier foreland of Midtre Lovénbreen. Soil samples (n = 45) were categorized by age based on exposure to the atmosphere due to glacier retreat in July 2014 into five age groups: 80-100 years (n = 7), 60-80 years (n = 12), 40-60 years (n = 16), 20-40 years (n = 7), and <20 years (n = 3). Concentrations of polychlorinated biphenyls (PCBs, n = 32) in soils varied with age, ranging from 0.29 to 0.74 ng g-1 dw. In addition, the concentrations of polycyclic aromatic hydrocarbons (PAHs, n = 28), perylene, and alkyl-PAHs (n = 20) in soils ranged from 21 to 80 ng g-1 dw, 2.9-62 ng g-1 dw, and 73-420 ng g-1 dw, respectively. The concentrations of PTSs were observed to be greater in older soils. Principal component analysis revealed that PCBs in soils originated from various product sources. Positive matrix factorization modeling estimated the association of PAHs in soils with potential origins, such as diesel emissions, petroleum and coal combustion, and coal. Potential sources of PAHs were mainly coal in younger soils and diesel emissions and petroleum combustion in older soils. Alkyl-PAH compositions in the soil were similar to those of bituminous coal, with a noteworthy degree of weathering observed in older soils. The accumulation rate and flux of PTSs in soils exhibited compound-specific patterns, reflecting factors such as long-range transport, fate, origin, and recent inputs. These findings can serve as baseline data for protecting and preserving polar environments.
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Affiliation(s)
- Jihyun Cha
- Department of Earth, Environmental & Space Sciences, Chungnam National University, Daejeon, 34134, Republic of Korea
| | - Jung-Hyun Kim
- Division of Glacier and Earth Sciences, Korea Polar Research Institute, Incheon, 21990, Republic of Korea
| | - Ji Young Jung
- Division of Life Sciences, Korea Polar Research Institute, Incheon, 21990, Republic of Korea
| | - Seung-Il Nam
- Division of Glacier and Earth Sciences, Korea Polar Research Institute, Incheon, 21990, Republic of Korea
| | - Seongjin Hong
- Department of Earth, Environmental & Space Sciences, Chungnam National University, Daejeon, 34134, Republic of Korea; Department of Marine Environmental Sciences, Chungnam National University, Daejeon, 34134, Republic of Korea.
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Ficetola GF, Marta S, Guerrieri A, Cantera I, Bonin A, Cauvy-Fraunié S, Ambrosini R, Caccianiga M, Anthelme F, Azzoni RS, Almond P, Alviz Gazitúa P, Ceballos Lievano JL, Chand P, Chand Sharma M, Clague JJ, Cochachín Rapre JA, Compostella C, Encarnación RC, Dangles O, Deline P, Eger A, Erokhin S, Franzetti A, Gielly L, Gili F, Gobbi M, Hågvar S, Kaufmann R, Khedim N, Meneses RI, Morales-Martínez MA, Peyre G, Pittino F, Proietto A, Rabatel A, Sieron K, Tielidze L, Urseitova N, Yang Y, Zaginaev V, Zerboni A, Zimmer A, Diolaiuti GA, Taberlet P, Poulenard J, Fontaneto D, Thuiller W, Carteron A. The development of terrestrial ecosystems emerging after glacier retreat. Nature 2024; 632:336-342. [PMID: 39085613 DOI: 10.1038/s41586-024-07778-2] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/18/2023] [Accepted: 07/02/2024] [Indexed: 08/02/2024]
Abstract
The global retreat of glaciers is dramatically altering mountain and high-latitude landscapes, with new ecosystems developing from apparently barren substrates1-4. The study of these emerging ecosystems is critical to understanding how climate change interacts with microhabitat and biotic communities and determines the future of ice-free terrains1,5. Here, using a comprehensive characterization of ecosystems (soil properties, microclimate, productivity and biodiversity by environmental DNA metabarcoding6) across 46 proglacial landscapes worldwide, we found that all the environmental properties change with time since glaciers retreated, and that temperature modulates the accumulation of soil nutrients. The richness of bacteria, fungi, plants and animals increases with time since deglaciation, but their temporal patterns differ. Microorganisms colonized most rapidly in the first decades after glacier retreat, whereas most macroorganisms took longer. Increased habitat suitability, growing complexity of biotic interactions and temporal colonization all contribute to the increase in biodiversity over time. These processes also modify community composition for all the groups of organisms. Plant communities show positive links with all other biodiversity components and have a key role in ecosystem development. These unifying patterns provide new insights into the early dynamics of deglaciated terrains and highlight the need for integrated surveillance of their multiple environmental properties5.
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Affiliation(s)
- Gentile Francesco Ficetola
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy.
- University of Grenoble Alpes, University of Savoie Mont Blanc, CNRS, LECA, Grenoble, France.
| | - Silvio Marta
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy.
- CNR - Institute of Geosciences and Earth Resources, Pisa, Italy.
| | - Alessia Guerrieri
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy
- Argaly, Bâtiment CleanSpace, Sainte-Hélène-du-Lac, France
| | - Isabel Cantera
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy
| | - Aurélie Bonin
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy
- Argaly, Bâtiment CleanSpace, Sainte-Hélène-du-Lac, France
| | | | - Roberto Ambrosini
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy
| | - Marco Caccianiga
- Dipartimento di Bioscienze, Università degli Studi di Milano, Milan, Italy
| | - Fabien Anthelme
- AMAP, University of Montpellier, IRD, CIRAD, CNRS, INRAE, Montpellier, France
| | - Roberto Sergio Azzoni
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy
- Dipartimento di Scienze della Terra "Ardito Desio", Università degli Studi di Milano, Milan, Italy
| | - Peter Almond
- Department of Soil and Physical Sciences, Lincoln University, Lincoln, New Zealand
| | - Pablo Alviz Gazitúa
- Departamento de Ciencias Biológicas y Biodiversidad, Universidad de Los Lagos, Osorno, Chile
| | | | - Pritam Chand
- Department of Geography, School of Environment and Earth Sciences, Central University of Punjab, VPO-Ghudda, Bathinda, India
| | - Milap Chand Sharma
- Centre for the Study of Regional Development, School of Social Sciences, Jawaharlal Nehru University, New Delhi, India
| | - John J Clague
- Department of Earth Sciences, Simon Fraser University, Burnaby, British Colombia, Canada
| | | | - Chiara Compostella
- Dipartimento di Scienze della Terra "Ardito Desio", Università degli Studi di Milano, Milan, Italy
| | | | - Olivier Dangles
- CEFE, University of Montpellier, CNRS, EPHE, IRD, University of Paul Valéry Montpellier 3, Montpellier, France
| | - Philip Deline
- University of Savoie Mont Blanc, University of Grenoble Alpes, EDYTEM, Chambéry, France
| | - Andre Eger
- Mannaki Whenua - Landcare Research, Soils and Landscapes, Lincoln, New Zealand
| | - Sergey Erokhin
- Institute of Water Problems and Hydro-Energy, Kyrgyz National Academy of Sciences, Bishkek, Kyrgyzstan
| | - Andrea Franzetti
- Department of Earth and Environmental Sciences (DISAT), University of Milano-Bicocca, Milan, Italy
| | - Ludovic Gielly
- University of Grenoble Alpes, University of Savoie Mont Blanc, CNRS, LECA, Grenoble, France
| | - Fabrizio Gili
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy
- Department of Life Sciences and Systems Biology, University of Turin, Turin, Italy
| | - Mauro Gobbi
- Research and Museum Collections Office, Climate and Ecology Unit, MUSE-Science Museum, Trento, Italy
| | - Sigmund Hågvar
- Faculty of Environmental Sciences and Natural Resource Management (INA), Norwegian University of Life Sciences, Ås, Norway
| | - Rüdiger Kaufmann
- Department of Ecology, University of Innsbruck, Innsbruck, Austria
| | - Norine Khedim
- University of Savoie Mont Blanc, University of Grenoble Alpes, EDYTEM, Chambéry, France
| | - Rosa Isela Meneses
- Herbario Nacional de Bolivia: La Paz, La Paz, Bolivia
- Millenium Nucleus in Andean Peatlands, Arica, Chile
| | | | - Gwendolyn Peyre
- Department of Civil and Environmental Engineering, University of the Andes, Bogotá, Colombia
| | - Francesca Pittino
- Department of Earth and Environmental Sciences (DISAT), University of Milano-Bicocca, Milan, Italy
- Swiss Federal Institute for Forest, Snow and Landscape Research, Birmensdorf, Switzerland
| | - Angela Proietto
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy
| | - Antoine Rabatel
- University of Grenoble Alpes, CNRS, IRD, INRAE, Grenoble-INP, Institut des Géosciences de l'Environnement (IGE UMR 5001), Grenoble, France
| | - Katrin Sieron
- Universidad Veracruzana, Centro de Ciencias de la Tierra, Xalapa, Veracruz, Mexico
| | - Levan Tielidze
- Securing Antarctica's Environmental Future, School of Earth, Atmosphere and Environment, Monash University, Clayton, Victoria, Australia
- School of Natural Sciences and Medicine, Ilia State University, Tbilisi, Georgia
| | - Nurai Urseitova
- Institute of Water Problems and Hydro-Energy, Kyrgyz National Academy of Sciences, Bishkek, Kyrgyzstan
| | - Yan Yang
- Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, China
| | - Vitalii Zaginaev
- Institute of Water Problems and Hydro-Energy, Kyrgyz National Academy of Sciences, Bishkek, Kyrgyzstan
- Mountain Societies Research Institute, University of Central Asia, Bishkek, Kyrgyzstan
| | - Andrea Zerboni
- Dipartimento di Scienze della Terra "Ardito Desio", Università degli Studi di Milano, Milan, Italy
| | - Anaïs Zimmer
- Department of Geography and the Environment, University of Texas at Austin, Austin, TX, USA
| | | | - Pierre Taberlet
- University of Grenoble Alpes, University of Savoie Mont Blanc, CNRS, LECA, Grenoble, France
- UiT - The Arctic University of Norway, Tromsø Museum, Tromsø, Norway
| | - Jerome Poulenard
- University of Savoie Mont Blanc, University of Grenoble Alpes, EDYTEM, Chambéry, France
| | - Diego Fontaneto
- CNR - Water Research Institute, Verbania, Italy
- NBFC - National Biodiversity Future Center, Palermo, Italy
| | - Wilfried Thuiller
- University of Grenoble Alpes, University of Savoie Mont Blanc, CNRS, LECA, Grenoble, France
| | - Alexis Carteron
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milan, Italy.
- Université de Toulouse, École d'Ingénieurs de PURPAN, UMR INRAE-INPT DYNAFOR, Toulouse, France.
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5
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Carteron A, Cantera I, Guerrieri A, Marta S, Bonin A, Ambrosini R, Anthelme F, Azzoni RS, Almond P, Alviz Gazitúa P, Cauvy-Fraunié S, Ceballos Lievano JL, Chand P, Chand Sharma M, Clague JJ, Cochachín Rapre JA, Compostella C, Cruz Encarnación R, Dangles O, Eger A, Erokhin S, Franzetti A, Gielly L, Gili F, Gobbi M, Hågvar S, Khedim N, Meneses RI, Peyre G, Pittino F, Rabatel A, Urseitova N, Yang Y, Zaginaev V, Zerboni A, Zimmer A, Taberlet P, Diolaiuti GA, Poulenard J, Thuiller W, Caccianiga M, Ficetola GF. Dynamics and drivers of mycorrhizal fungi after glacier retreat. THE NEW PHYTOLOGIST 2024; 242:1739-1752. [PMID: 38581206 DOI: 10.1111/nph.19682] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/31/2023] [Accepted: 12/17/2023] [Indexed: 04/08/2024]
Abstract
The development of terrestrial ecosystems depends greatly on plant mutualists such as mycorrhizal fungi. The global retreat of glaciers exposes nutrient-poor substrates in extreme environments and provides a unique opportunity to study early successions of mycorrhizal fungi by assessing their dynamics and drivers. We combined environmental DNA metabarcoding and measurements of local conditions to assess the succession of mycorrhizal communities during soil development in 46 glacier forelands around the globe, testing whether dynamics and drivers differ between mycorrhizal types. Mycorrhizal fungi colonized deglaciated areas very quickly (< 10 yr), with arbuscular mycorrhizal fungi tending to become more diverse through time compared to ectomycorrhizal fungi. Both alpha- and beta-diversity of arbuscular mycorrhizal fungi were significantly related to time since glacier retreat and plant communities, while microclimate and primary productivity were more important for ectomycorrhizal fungi. The richness and composition of mycorrhizal communities were also significantly explained by soil chemistry, highlighting the importance of microhabitat for community dynamics. The acceleration of ice melt and the modifications of microclimate forecasted by climate change scenarios are expected to impact the diversity of mycorrhizal partners. These changes could alter the interactions underlying biotic colonization and belowground-aboveground linkages, with multifaceted impacts on soil development and associated ecological processes.
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Affiliation(s)
- Alexis Carteron
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Via Celoria 10, 20133, Milano, Italy
- Université de Toulouse, Ecole d'Ingénieurs de PURPAN, UMR INRAE-INPT DYNAFOR, Toulouse, 31076, France
| | - Isabel Cantera
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Via Celoria 10, 20133, Milano, Italy
| | - Alessia Guerrieri
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Via Celoria 10, 20133, Milano, Italy
- Argaly, Bâtiment CleanSpace, 354 Voie Magellan, 73800, Sainte-Hélène-du-Lac, France
| | - Silvio Marta
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Via Celoria 10, 20133, Milano, Italy
- Institute of Geosciences and Earth Resources, CNR, Via Moruzzi 1, 56124, Pisa, Italy
| | - Aurélie Bonin
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Via Celoria 10, 20133, Milano, Italy
- Argaly, Bâtiment CleanSpace, 354 Voie Magellan, 73800, Sainte-Hélène-du-Lac, France
| | - Roberto Ambrosini
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Via Celoria 10, 20133, Milano, Italy
| | - Fabien Anthelme
- AMAP, Univ Montpellier, IRD, CIRAD, CNRS, INRAE, Montpellier, 34398, France
| | - Roberto Sergio Azzoni
- Dipartimento di Scienze della Terra 'Ardito Desio', Università degli Studi di Milano, Via L. Mangiagalli 34, 20133, Milano, Italy
| | - Peter Almond
- Department of Soil and Physical Sciences, Lincoln University, Lincoln, 7647, New Zealand
| | - Pablo Alviz Gazitúa
- Departamento de Ciencias Biológicas y Biodiversidad, Universidad de Los Lagos, CW76+76, Osorno, Chile
| | | | | | - Pritam Chand
- Department of Geography, School of Environment and Earth Sciences, Central University of Punjab, VPO-Ghudda, Bathinda, 151401, Punjab, India
| | - Milap Chand Sharma
- Centre for the Study of Regional Development - School of Social Sciences, Jawaharlal Nehru University, New Mehrauli Road, 110067, New Delhi, India
| | - John J Clague
- Department of Earth Sciences, Simon Fraser University, 8888 University Drive, Burnaby, BC, V5A 1S6, Canada
| | | | - Chiara Compostella
- Dipartimento di Scienze della Terra 'Ardito Desio', Università degli Studi di Milano, Via L. Mangiagalli 34, 20133, Milano, Italy
| | | | - Olivier Dangles
- CEFE, Univ Montpellier, CNRS, EPHE, IRD, Univ Paul Valéry Montpellier 3, 34090, Montpellier, France
| | - Andre Eger
- Mannaki Whenua - Landcare Research, Soils and Landscapes, 54 Gerald St., Lincoln, 7608, New Zealand
| | - Sergey Erokhin
- Institute of Water Problems and Hydro-Energy, Kyrgyz National Academy of Sciences, Frunze, 533, 720033, Bishkek, Kyrgyzstan
| | - Andrea Franzetti
- Department of Earth and Environmental Sciences (DISAT), University of Milano-Bicocca, 20126, Milano, Italy
| | - Ludovic Gielly
- Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, LECA, F-38000, Grenoble, France
| | - Fabrizio Gili
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Via Celoria 10, 20133, Milano, Italy
- Department of Life Sciences and Systems Biology, University of Turin, Via Accademia Albertina 13, 10123, Turin, Italy
| | - Mauro Gobbi
- Research and Museum Collections Office, Climate and Ecology Unit, MUSE-Science Museum, Corso del Lavoro e della Scienza, 3, 38122, Trento, Italy
| | - Sigmund Hågvar
- Faculty of Environmental Sciences and Natural Resource Management (INA), Norwegian University of Life Sciences, Universitetstunet 3, 1433, Ås, Norway
- UiT - The Arctic University of Norway, Tromsø Museum, Tromsø, 9006, Norway
| | - Norine Khedim
- Université Savoie Mont Blanc, Université Grenoble Alpes, EDYTEM, F-73000, Chambéry, France
| | - Rosa Isela Meneses
- Herbario Nacional de Bolivia: La Paz, FW6J+RP2, La Paz, Bolivia
- Universidad Católica del Norte, 8HCR+94, Antofagasta, Chile
| | - Gwendolyn Peyre
- Department of Civil and Environmental Engineering, University of the Andes, 111711, Bogotá, Colombia
| | - Francesca Pittino
- Department of Earth and Environmental Sciences (DISAT), University of Milano-Bicocca, 20126, Milano, Italy
- Swiss Federal Institute for Forest, Snow and Landscape Research, Zürcherstrasse 111, 8903, Birmensdorf, Switzerland
| | - Antoine Rabatel
- Université Grenoble Alpes, CNRS, IRD, INRAE, Grenoble-INP, Institut des Géosciences de l'Environnement (IGE, UMR 5001), F-38000, Grenoble, France
| | - Nurai Urseitova
- Institute of Water Problems and Hydro-Energy, Kyrgyz National Academy of Sciences, Frunze, 533, 720033, Bishkek, Kyrgyzstan
| | - Yan Yang
- Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, 610041, China
| | - Vitalii Zaginaev
- Mountain Societies Research Institute, University of Central Asia, Toktogula 125/1, 720001, Bishkek, Kyrgyzstan
| | - Andrea Zerboni
- Dipartimento di Scienze della Terra 'Ardito Desio', Università degli Studi di Milano, Via L. Mangiagalli 34, 20133, Milano, Italy
| | - Anaïs Zimmer
- Department of Geography and the Environment, University of Texas at Austin, Austin, TX, 78712, USA
| | - Pierre Taberlet
- Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, LECA, F-38000, Grenoble, France
- UiT - The Arctic University of Norway, Tromsø Museum, Tromsø, 9006, Norway
| | - Guglielmina Adele Diolaiuti
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Via Celoria 10, 20133, Milano, Italy
| | - Jerome Poulenard
- Université Savoie Mont Blanc, Université Grenoble Alpes, EDYTEM, F-73000, Chambéry, France
| | - Wilfried Thuiller
- Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, LECA, F-38000, Grenoble, France
| | - Marco Caccianiga
- Dipartimento di Bioscienze, Universitá degli Studi di Milano, Via Celoria 26, 20133, Milano, Italy
| | - Gentile Francesco Ficetola
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Via Celoria 10, 20133, Milano, Italy
- Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, LECA, F-38000, Grenoble, France
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6
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Guerrieri A, Cantera I, Marta S, Bonin A, Carteron A, Ambrosini R, Caccianiga M, Anthelme F, Azzoni RS, Almond P, Alviz Gazitúa P, Cauvy-Fraunié S, Ceballos Lievano JL, Chand P, Chand Sharma M, Clague J, Cochachín Rapre JA, Compostella C, Cruz Encarnación R, Dangles O, Deline P, Eger A, Erokhin S, Franzetti A, Gielly L, Gili F, Gobbi M, Hågvar S, Khedim N, Meneses RI, Peyre G, Pittino F, Proietto A, Rabatel A, Urseitova N, Yang Y, Zaginaev V, Zerboni A, Zimmer A, Taberlet P, Diolaiuti GA, Poulenard J, Fontaneto D, Thuiller W, Ficetola GF. Local climate modulates the development of soil nematode communities after glacier retreat. GLOBAL CHANGE BIOLOGY 2024; 30:e17057. [PMID: 38273541 DOI: 10.1111/gcb.17057] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/27/2023] [Accepted: 10/10/2023] [Indexed: 01/27/2024]
Abstract
The worldwide retreat of glaciers is causing a faster than ever increase in ice-free areas that are leading to the emergence of new ecosystems. Understanding the dynamics of these environments is critical to predicting the consequences of climate change on mountains and at high latitudes. Climatic differences between regions of the world could modulate the emergence of biodiversity and functionality after glacier retreat, yet global tests of this hypothesis are lacking. Nematodes are the most abundant soil animals, with keystone roles in ecosystem functioning, but the lack of global-scale studies limits our understanding of how the taxonomic and functional diversity of nematodes changes during the colonization of proglacial landscapes. We used environmental DNA metabarcoding to characterize nematode communities of 48 glacier forelands from five continents. We assessed how different facets of biodiversity change with the age of deglaciated terrains and tested the hypothesis that colonization patterns are different across forelands with different climatic conditions. Nematodes colonized ice-free areas almost immediately. Both taxonomic and functional richness quickly increased over time, but the increase in nematode diversity was modulated by climate, so that colonization started earlier in forelands with mild summer temperatures. Colder forelands initially hosted poor communities, but the colonization rate then accelerated, eventually leveling biodiversity differences between climatic regimes in the long term. Immediately after glacier retreat, communities were dominated by colonizer taxa with short generation time and r-ecological strategy but community composition shifted through time, with increased frequency of more persister taxa with K-ecological strategy. These changes mostly occurred through the addition of new traits instead of their replacement during succession. The effects of local climate on nematode colonization led to heterogeneous but predictable patterns around the world that likely affect soil communities and overall ecosystem development.
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Affiliation(s)
- Alessia Guerrieri
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milano, Italy
- Argaly, Bâtiment CleanSpace, Sainte-Hélène-du-Lac, France
| | - Isabel Cantera
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milano, Italy
| | - Silvio Marta
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milano, Italy
- Institute of Geosciences and Earth Resources, CNR, Pisa, Italy
| | - Aurélie Bonin
- Argaly, Bâtiment CleanSpace, Sainte-Hélène-du-Lac, France
| | - Alexis Carteron
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milano, Italy
| | - Roberto Ambrosini
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milano, Italy
| | - Marco Caccianiga
- Dipartimento di Bioscienze, Università degli Studi di Milano, Milano, Italy
| | - Fabien Anthelme
- Laboratory AMAP, IRD, University of Montpellier, CIRAD, CNRS, INRA, Montpellier, France
| | - Roberto Sergio Azzoni
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milano, Italy
- Dipartimento di Scienze della Terra "Ardito Desio", Università degli Studi di Milano, Milano, Italy
| | - Peter Almond
- Department of Soil and Physical Sciences, Lincoln University, Lincoln, New Zealand
| | - Pablo Alviz Gazitúa
- Departamento de Ciencias Biológicas y Biodiversidad, Universidad de Los Lagos, Osorno, Chile
| | | | | | - Pritam Chand
- Department of Geography, School of Environment and Earth Sciences, Central University of Punjab, Bathinda, Punjab, India
| | - Milap Chand Sharma
- Centre for the Study of Regional Development - School of Social Sciences, Jawaharlal Nehru University, New Delhi, India
| | - John Clague
- Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia, Canada
| | | | - Chiara Compostella
- Dipartimento di Scienze della Terra "Ardito Desio", Università degli Studi di Milano, Milano, Italy
| | | | - Olivier Dangles
- CEFE, Univ Montpellier, CNRS, EPHE, IRD, Univ Paul Valéry Montpellier 3, Montpellier, France
| | - Philip Deline
- Univ. Savoie Mont Blanc, Univ. Grenoble Alpes, EDYTEM, Chambéry, France
| | - Andre Eger
- Mannaki Whenua - Landcare Research, Soils and Landscapes, Lincoln, New Zealand
| | - Sergey Erokhin
- Institute of Water Problems and Hydro-Energy, Kyrgyz National Academy of Sciences, Bishkek, Kyrgyzstan
| | - Andrea Franzetti
- Department of Earth and Environmental Sciences (DISAT), University of Milano-Bicocca, Milano, Italy
| | - Ludovic Gielly
- Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, LECA, Grenoble, France
| | - Fabrizio Gili
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milano, Italy
- Department of Life Sciences and Systems Biology, University of Turin, Turin, Italy
| | - Mauro Gobbi
- Research and Museum Collections Office, Climate and Ecology Unit, MUSE-Science Museum, Corso del Lavoro e della Scienza, Trento, Italy
| | - Sigmund Hågvar
- Faculty of Environmental Sciences and Natural Resource Management (INA), Norwegian University of Life Sciences, Ås, Norway
- UiT - The Arctic University of Norway, Tromsø Museum, Tromsø, Norway
| | - Norine Khedim
- Univ. Savoie Mont Blanc, Univ. Grenoble Alpes, EDYTEM, Chambéry, France
| | - Rosa Isela Meneses
- Herbario Nacional de Bolivia: La Paz, La Paz, Bolivia
- Universidad Católica del Norte, Antofagasta, Chile
| | - Gwendolyn Peyre
- Department of Civil and Environmental Engineering, University of the Andes, Bogotá, Colombia
| | - Francesca Pittino
- Department of Earth and Environmental Sciences (DISAT), University of Milano-Bicocca, Milano, Italy
| | - Angela Proietto
- Dipartimento di Scienze della Terra "Ardito Desio", Università degli Studi di Milano, Milano, Italy
| | - Antoine Rabatel
- Univ. Grenoble Alpes, CNRS, IRD, Grenoble-INP, Institut des Géosciences de l'Environnement (IGE, UMR 5001), Grenoble, France
| | - Nurai Urseitova
- Institute of Water Problems and Hydro-Energy, Kyrgyz National Academy of Sciences, Bishkek, Kyrgyzstan
| | - Yan Yang
- Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, China
| | - Vitalii Zaginaev
- Mountain Societies Research Institute, University of Central Asia, Bishkek, Kyrgyzstan
| | - Andrea Zerboni
- Dipartimento di Scienze della Terra "Ardito Desio", Università degli Studi di Milano, Milano, Italy
| | - Anaïs Zimmer
- Department of Geography and the Environment, University of Texas at Austin, Austin, Texas, USA
| | - Pierre Taberlet
- Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, LECA, Grenoble, France
- UiT - The Arctic University of Norway, Tromsø Museum, Tromsø, Norway
| | | | - Jerome Poulenard
- Univ. Savoie Mont Blanc, Univ. Grenoble Alpes, EDYTEM, Chambéry, France
| | - Diego Fontaneto
- CNR - Water Research Institute, Verbania, Italy
- NBFC - National Biodiversity Future Center, Palermo, Italy
| | - Wilfried Thuiller
- Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, LECA, Grenoble, France
| | - Gentile Francesco Ficetola
- Dipartimento di Scienze e Politiche Ambientali, Università degli Studi di Milano, Milano, Italy
- Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, LECA, Grenoble, France
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7
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Marchal L, Gateuille D, Naffrechoux E, Deline P, Baudin F, Clément JC, Poulenard J. Polycyclic aromatic hydrocarbon dynamics in soils along proglacial chronosequences in the Alps. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 902:165998. [PMID: 37536589 DOI: 10.1016/j.scitotenv.2023.165998] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/14/2023] [Revised: 07/31/2023] [Accepted: 07/31/2023] [Indexed: 08/05/2023]
Abstract
Polycyclic aromatic hydrocarbons (PAHs) were studied in the soils of three proglacial areas in France (Noir and Chardon Glaciers) and Italy (Miage Glacier). PAH contents, PAH stocks and PAH contents normalized to the total organic carbon contents (PAHs/TOC ratio) were investigated along proglacial soil chronosequences to infer their evolutions with soil age (from 3 to 4200 years), where the PAH contamination was only related to long-range atmospheric transport. Evolutions of PAH and TOC contents, PAHs/TOC ratio and PAH stock were fitted with exponential and logarithmic relations. For the three proglacial areas, PAH contents increased rapidly during the first 150 years of soil development, ranged from 4 to 152 ng·g-1, and showed a strong relationship with total organic carbon (TOC) contents (r = 0.83, p < 0.05). The joint increase of PAH and TOC contents suggested that PAH accumulation in soils were not only driven by PAH inputs but also by the capacity of soils to store these contaminants. PAH contents in the oldest soils (from 1200 BCE and 2200 BCE) were similar than for soils from 1850 CE. The period 1850-2019 CE corresponded to a decrease in the PAHs/TOC ratio suggesting both a faster accumulation of TOC than PAHs and a dilution effect of PAHs already present in soils. For the oldest soils, the PAHs/TOC ratio appeared similar to those for soils from 1850 CE, with values ranging from 0.48 to 2.06 ng·mg-1, suggesting an equilibrium between both parameters for soils older than 170 years. Finally, PAH stocks ranged from 0.41 mg·m-2 to 6.80 mg·m-2 in the youngest and oldest soils, respectively. These results do not allow us to identify the same period of greatest emission as other studies (estimated ~1960), but they revealed changes in the capacity of soils to store these pollutants.
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Affiliation(s)
- Lise Marchal
- Savoie Mont-Blanc University, CNRS, EDYTEM, 73000 Chambéry, France.
| | - David Gateuille
- Savoie Mont-Blanc University, CNRS, EDYTEM, 73000 Chambéry, France
| | | | - Philip Deline
- Savoie Mont-Blanc University, CNRS, EDYTEM, 73000 Chambéry, France
| | | | | | - Jérôme Poulenard
- Savoie Mont-Blanc University, CNRS, EDYTEM, 73000 Chambéry, France
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8
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Feng M, Varliero G, Qi W, Stierli B, Edwards A, Robinson S, van der Heijden MGA, Frey B. Microbial dynamics in soils of the Damma glacier forefield show succession in the functional genetic potential. Environ Microbiol 2023; 25:3116-3138. [PMID: 37688461 DOI: 10.1111/1462-2920.16497] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/29/2023] [Accepted: 08/08/2023] [Indexed: 09/10/2023]
Abstract
Glacier retreat is a visible consequence of climate change worldwide. Although taxonomic change of the soil microbiomes in glacier forefields have been widely documented, how microbial genetic potential changes along succession is little known. Here, we used shotgun metagenomics to analyse whether the soil microbial genetic potential differed between four stages of soil development (SSD) sampled along three transects in the Damma glacier forefield (Switzerland). The SSDs were characterized by an increasing vegetation cover, from barren soil, to biological soil crust, to sparsely vegetated soil and finally to vegetated soil. Results suggested that SSD significantly influenced microbial genetic potential, with the lowest functional diversity surprisingly occurring in the vegetated soils. Overall, carbohydrate metabolism and secondary metabolite biosynthesis genes overrepresented in vegetated soils, which could be partly attributed to plant-soil feedbacks. For C degradation, glycoside hydrolase genes enriched in vegetated soils, while auxiliary activity and carbohydrate esterases genes overrepresented in barren soils, suggested high labile C degradation potential in vegetated, and high recalcitrant C degradation potential in barren soils. For N-cycling, organic N degradation and synthesis genes dominated along succession, and gene families involved in nitrification were overrepresented in barren soils. Our study provides new insights into how the microbial genetic potential changes during soil formation along the Damma glacier forefield.
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Affiliation(s)
- Maomao Feng
- Rhizosphere Processes Group, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland
- Department of Plant and Microbial Biology, University of Zurich, Zurich, Switzerland
| | - Gilda Varliero
- Rhizosphere Processes Group, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland
| | - Weihong Qi
- Functional Genomics Center Zurich, ETH Zurich and University of Zurich, Zurich, Switzerland
- Swiss Institute of Bioinformatics SIB, Geneva, Switzerland
| | - Beat Stierli
- Rhizosphere Processes Group, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland
| | - Arwyn Edwards
- Institute of Biological, Environmental and Rural Sciences, Aberystwyth University, Aberystwyth, UK
| | - Serina Robinson
- Department of Environmental Microbiology, Swiss Federal Institute of Aquatic Science and Technology (EAWAG), Dübendorf, Switzerland
| | - Marcel G A van der Heijden
- Department of Plant and Microbial Biology, University of Zurich, Zurich, Switzerland
- Plant-Soil Interactions, Agroscope, Zurich, Switzerland
| | - Beat Frey
- Rhizosphere Processes Group, Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland
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9
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Guerrieri A, Carteron A, Bonin A, Marta S, Ambrosini R, Caccianiga M, Cantera I, Compostella C, Diolaiuti G, Fontaneto D, Gielly L, Gili F, Gobbi M, Poulenard J, Taberlet P, Zerboni A, Thuiller W, Ficetola GF. Metabarcoding data reveal vertical multitaxa variation in topsoil communities during the colonization of deglaciated forelands. Mol Ecol 2023; 32:6304-6319. [PMID: 35997629 DOI: 10.1111/mec.16669] [Citation(s) in RCA: 6] [Impact Index Per Article: 6.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/23/2021] [Revised: 07/21/2022] [Accepted: 08/15/2022] [Indexed: 11/27/2022]
Abstract
Ice-free areas are expanding worldwide due to dramatic glacier shrinkage and are undergoing rapid colonization by multiple lifeforms, thus representing key environments to study ecosystem development. It has been proposed that the colonization dynamics of deglaciated terrains is different between surface and deep soils but that the heterogeneity between communities inhabiting surface and deep soils decreases through time. Nevertheless, tests of this hypothesis remain scarce, and it is unclear whether patterns are consistent among different taxonomic groups. Here, we used environmental DNA metabarcoding to test whether community diversity and composition of six groups (Eukaryota, Bacteria, Mycota, Collembola, Insecta, and Oligochaeta) differ between the surface (0-5 cm) and deeper (7.5-20 cm) soil at different stages of development and across five Alpine glaciers. Taxonomic diversity increased with time since glacier retreat and with soil evolution. The pattern was consistent across groups and soil depths. For Eukaryota and Mycota, alpha-diversity was highest at the surface. Time since glacier retreat explained more variation of community composition than depth. Beta-diversity between surface and deep layers decreased with time since glacier retreat, supporting the hypothesis that the first 20 cm of soil tends to homogenize through time. Several molecular operational taxonomic units of bacteria and fungi were significant indicators of specific depths and/or soil development stages, confirming the strong functional variation of microbial communities through time and depth. The complexity of community patterns highlights the importance of integrating information from multiple taxonomic groups to unravel community variation in response to ongoing global changes.
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Affiliation(s)
- Alessia Guerrieri
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
| | - Alexis Carteron
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
| | - Aurélie Bonin
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
- Argaly, Bâtiment CleanSpace, Sainte-Hélène-du-Lac, France
| | - Silvio Marta
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
| | - Roberto Ambrosini
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
| | - Marco Caccianiga
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
| | - Isabel Cantera
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
| | - Chiara Compostella
- Department of Earth Sciences, "A. Desio," Università degli Studi di Milano, Milan, Italy
| | - Guglielmina Diolaiuti
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
| | | | - Ludovic Gielly
- Univ. Grenoble Alpes, CNRS, Univ. Savoie Mont Blanc, LECA, Laboratoire d'Ecologie Alpine, Grenoble, France
| | - Fabrizio Gili
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
| | - Mauro Gobbi
- Research & Museum Collections Office, Climate and Ecology Unit, MUSE-Science Museum, Trento, Italy
| | | | - Pierre Taberlet
- Univ. Grenoble Alpes, CNRS, Univ. Savoie Mont Blanc, LECA, Laboratoire d'Ecologie Alpine, Grenoble, France
- UiT - The Arctic University of Norway, Tromsø Museum, Tromsø, Norway
| | - Andrea Zerboni
- Department of Earth Sciences, "A. Desio," Università degli Studi di Milano, Milan, Italy
| | - Wilfried Thuiller
- Univ. Grenoble Alpes, CNRS, Univ. Savoie Mont Blanc, LECA, Laboratoire d'Ecologie Alpine, Grenoble, France
| | - Gentile Francesco Ficetola
- Department of Environmental Science and Policy, Università degli Studi di Milano, Milan, Italy
- Univ. Grenoble Alpes, CNRS, Univ. Savoie Mont Blanc, LECA, Laboratoire d'Ecologie Alpine, Grenoble, France
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10
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Zimmer A, Beach T, Riva Regalado S, Salcedo Aliaga J, Cruz Encarnación R, Anthelme F. Llamas (Llama glama) enhance proglacial ecosystem development in Cordillera Blanca, Peru. Sci Rep 2023; 13:15936. [PMID: 37743358 PMCID: PMC10518316 DOI: 10.1038/s41598-023-41458-x] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/15/2023] [Accepted: 08/27/2023] [Indexed: 09/26/2023] Open
Abstract
Worldwide, mountain glaciers are shrinking rapidly. Consequently, large areas are becoming available for the development of novel alpine ecosystems. These harsh environments, however, delay primary succession. In this study with a local community, we conducted an inclusion experiment to investigate whether Llama glama influences soils and vegetation primary succession following glacial retreat. At the foot of the Uruashraju glacier in the Cordillera Blanca, Peru (~ 4680 m.a.s.l.), we established four llama inclusion plots and four control plots that we studied from 2019 to 2022, 24-40 years after deglacierization. After three years, the llama plots had significantly increased soil organic carbon and soil nitrogen. In the llama plots, we found a large, significant increase in vascular plant cover (+ 57%) between the second and third years of experimentation, and we identified four new species that were not present in 2019. Our results suggest that Llama glama, through their latrine behavior and role as a seed disperser, enhances the primary succession and novel ecosystem formation in recently deglacierized landscapes. Our study provides scientific support that rewilding of native Andean camelids may favor adaptation to glacier retreat and inform conservation and management strategies in proglacial landscapes.
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Affiliation(s)
- Anaïs Zimmer
- Department of Geography and the Environment, University of Texas at Austin, Austin, TX, USA.
| | - Timothy Beach
- Department of Geography and the Environment, University of Texas at Austin, Austin, TX, USA
| | - Sebastián Riva Regalado
- Laboratorio de Florística, Departamento de Dicotiledóneas, Museo de Historia Natural, Universidad Nacional Mayor de San Marcos, Lima, Peru
| | - Jean Salcedo Aliaga
- Departamento de Etnobotánica y Botánica Económica, Museo de Historia Natural. Universidad Nacional Mayor de San Marcos, Lima, Peru
| | - Rolando Cruz Encarnación
- Área de Evaluación de Glaciares y Lagunas, Autoridad Nacional del Agua, Huaraz, Peru
- Universidad Nacional Santiago Antúnez de Mayolo, Huaraz, Peru
| | - Fabien Anthelme
- AMAP, Univ Montpellier, IRD, CIRAD, CNRS, INRAE, Montpellier, France
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11
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Marta S, Zimmer A, Caccianiga M, Gobbi M, Ambrosini R, Azzoni RS, Gili F, Pittino F, Thuiller W, Provenzale A, Ficetola GF. Heterogeneous changes of soil microclimate in high mountains and glacier forelands. Nat Commun 2023; 14:5306. [PMID: 37652908 PMCID: PMC10471727 DOI: 10.1038/s41467-023-41063-6] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/27/2022] [Accepted: 08/22/2023] [Indexed: 09/02/2023] Open
Abstract
Landscapes nearby glaciers are disproportionally affected by climate change, but we lack detailed information on microclimate variations that can modulate the impacts of global warming on proglacial ecosystems and their biodiversity. Here, we use near-subsurface soil temperatures in 175 stations from polar, equatorial and alpine glacier forelands to generate high-resolution temperature reconstructions, assess spatial variability in microclimate change from 2001 to 2020, and estimate whether microclimate heterogeneity might buffer the severity of warming trends. Temporal changes in microclimate are tightly linked to broad-scale conditions, but the rate of local warming shows great spatial heterogeneity, with faster warming nearby glaciers and during the warm season, and an extension of the snow-free season. Still, most of the fine-scale spatial variability of microclimate is one-to-ten times larger than the temporal change experienced during the past 20 years, indicating the potential for microclimate to buffer climate change, possibly allowing organisms to withstand, at least temporarily, the effects of warming.
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Affiliation(s)
- Silvio Marta
- Department of Environmental Science and Policy, University of Milan, Via G. Celoria 10, 20133, Milan, Italy.
- Institute of Geosciences and Earth Resources, IGG-CNR, Italian National Research Council, 56124, Pisa, Italy.
| | - Anaïs Zimmer
- Department of Geography and the Environment, University of Texas at Austin, 78712, Austin, TX, USA
| | - Marco Caccianiga
- Department of Biosciences, University of Milan, via G. Celoria 26, 20133, Milan, Italy
| | - Mauro Gobbi
- Research & Museum Collections Office, Climate and Ecology Unit, MUSE-Science Museum, Corso del Lavoro e della Scienza 3, 38122, Trento, Italy
| | - Roberto Ambrosini
- Department of Environmental Science and Policy, University of Milan, Via G. Celoria 10, 20133, Milan, Italy
| | - Roberto Sergio Azzoni
- Department of Environmental Science and Policy, University of Milan, Via G. Celoria 10, 20133, Milan, Italy
- Department of Earth Sciences "Ardito Desio", University of Milan, Via L. Mangiagalli 34, 20133, Milan, Italy
| | - Fabrizio Gili
- Department of Environmental Science and Policy, University of Milan, Via G. Celoria 10, 20133, Milan, Italy
- Department of Life Sciences and Systems Biology, University of Turin, Via Accademia Albertina 13, 10123, Turin, Italy
| | - Francesca Pittino
- Department of Earth and Environmental Sciences (DISAT) - University of Milan-Bicocca, Milan, Italy
| | - Wilfried Thuiller
- Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, LECA, F38000, Grenoble, France
| | - Antonello Provenzale
- Institute of Geosciences and Earth Resources, IGG-CNR, Italian National Research Council, 56124, Pisa, Italy
| | - Gentile Francesco Ficetola
- Department of Environmental Science and Policy, University of Milan, Via G. Celoria 10, 20133, Milan, Italy
- Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, LECA, F38000, Grenoble, France
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12
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Bosson JB, Huss M, Cauvy-Fraunié S, Clément JC, Costes G, Fischer M, Poulenard J, Arthaud F. Future emergence of new ecosystems caused by glacial retreat. Nature 2023; 620:562-569. [PMID: 37587299 DOI: 10.1038/s41586-023-06302-2] [Citation(s) in RCA: 5] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/16/2023] [Accepted: 06/08/2023] [Indexed: 08/18/2023]
Abstract
Glacier shrinkage and the development of post-glacial ecosystems related to anthropogenic climate change are some of the fastest ongoing ecosystem shifts, with marked ecological and societal cascading consequences1-6. Yet, no complete spatial analysis exists, to our knowledge, to quantify or anticipate this important changeover7,8. Here we show that by 2100, the decline of all glaciers outside the Antarctic and Greenland ice sheets may produce new terrestrial, marine and freshwater ecosystems over an area ranging from the size of Nepal (149,000 ± 55,000 km2) to that of Finland (339,000 ± 99,000 km2). Our analysis shows that the loss of glacier area will range from 22 ± 8% to 51 ± 15%, depending on the climate scenario. In deglaciated areas, the emerging ecosystems will be characterized by extreme to mild ecological conditions, offering refuge for cold-adapted species or favouring primary productivity and generalist species. Exploring the future of glacierized areas highlights the importance of glaciers and emerging post-glacial ecosystems in the face of climate change, biodiversity loss and freshwater scarcity. We find that less than half of glacial areas are located in protected areas. Echoing the recent United Nations resolution declaring 2025 as the International Year of Glaciers' Preservation9 and the Global Biodiversity Framework10, we emphasize the need to urgently and simultaneously enhance climate-change mitigation and the in situ protection of these ecosystems to secure their existence, functioning and values.
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Affiliation(s)
- J B Bosson
- Asters, Conservatory of Natural Areas of Haute-Savoie, Annecy, France.
| | - M Huss
- Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland
- Laboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH Zürich, Zürich, Switzerland
- Department of Geosciences, University of Fribourg, Fribourg, Switzerland
| | - S Cauvy-Fraunié
- INRAE, UR RIVERLY, Centre de Lyon-Villeurbanne, Villeurbanne, France
| | - J C Clément
- Université Savoie Mont Blanc, INRAE, CARRTEL, Thonon-les-Bains, France
| | - G Costes
- Asters, Conservatory of Natural Areas of Haute-Savoie, Annecy, France
| | - M Fischer
- Institute of Geography, University of Bern, Bern, Switzerland
- Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
| | - J Poulenard
- Laboratory Environnement Dynamique et Territoire de la Montagne (EDYTEM), Université Savoie Mont Blanc, CNRS, Le Bourget-du-Lac, France
| | - F Arthaud
- Université Savoie Mont Blanc, INRAE, CARRTEL, Thonon-les-Bains, France
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13
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Yu S, Lv J, Jiang L, Geng P, Cao D, Wang Y. Changes of Soil Dissolved Organic Matter and Its Relationship with Microbial Community along the Hailuogou Glacier Forefield Chronosequence. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:4027-4038. [PMID: 36811997 DOI: 10.1021/acs.est.2c08855] [Citation(s) in RCA: 17] [Impact Index Per Article: 17.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/18/2023]
Abstract
Glacier-retreated areas are ideal areas to study soil biogeochemical processes during vegetation succession, because of the limited effect of other environmental and climatic factors. In this study, the changes of soil dissolved organic matter (DOM) and its relationship with microbial communities along the Hailuogou Glacier forefield chronosequence were investigated. Both microbial diversity and DOM molecular chemodiversity recovered rapidly at the initial stage, indicating the pioneering role of microorganisms in soil formation and development. The chemical stability of soil organic matter enhanced with vegetation succession due to the retaining of compounds with high oxidation state and aromaticity. The molecular composition of DOM affected microbial communities, while microorganisms tended to utilize labile components to form refractory components. This complex relationship network between microorganisms and DOM components played an important role in the development of soil organic matter as well as the formation of stable soil carbon pool in glacier-retreated areas.
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Affiliation(s)
- Shiyang Yu
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Jitao Lv
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Lu Jiang
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Pengyu Geng
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Dong Cao
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- University of Chinese Academy of Sciences, Beijing 100049, China
| | - Yawei Wang
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
- University of Chinese Academy of Sciences, Beijing 100049, China
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14
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Rolli E, Marasco R, Fusi M, Scaglia B, Schubotz F, Mapelli F, Ciccazzo S, Brusetti L, Trombino L, Tambone F, Adani F, Borin S, Daffonchio D. Environmental micro-niche filtering shapes bacterial pioneer communities during primary colonization of a Himalayas' glacier forefield. Environ Microbiol 2022; 24:5998-6016. [PMID: 36325730 PMCID: PMC10099744 DOI: 10.1111/1462-2920.16268] [Citation(s) in RCA: 5] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/25/2022] [Accepted: 10/27/2022] [Indexed: 11/06/2022]
Abstract
The pedogenesis from the mineral substrate released upon glacier melting has been explained with the succession of consortia of pioneer microorganisms, whose structure and functionality are determined by the environmental conditions developing in the moraine. However, the microbiome variability that can be expected in the environmentally heterogeneous niches occurring in a moraine at a given successional stage is poorly investigated. In a 50 m2 area in the forefield of the Lobuche glacier (Himalayas, 5050 m above sea level), we studied six sites of primary colonization presenting different topographical features (orientation, elevation and slope) and harbouring greyish/dark biological soil crusts (BSCs). The spatial vicinity of the sites opposed to their topographical differences, allowed us to examine the effect of environmental conditions independently from the time of deglaciation. The bacterial microbiome diversity and their co-occurrence network, the bacterial metabolisms predicted from 16S rRNA gene high-throughput sequencing, and the microbiome intact polar lipids were investigated in the BSCs and the underlying sediment deep layers (DLs). Different bacterial microbiomes inhabited the BSCs and the DLs, and their composition varied among sites, indicating a niche-specific role of the micro-environmental conditions in the bacterial communities' assembly. In the heterogeneous sediments of glacier moraines, physico-chemical and micro-climatic variations at the site-spatial scale are crucial in shaping the microbiome microvariability and structuring the pioneer bacterial communities during pedogenesis.
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Affiliation(s)
- Eleonora Rolli
- Department of Food, Environmental and Nutritional Sciences, University of Milan, Milan, Italy
| | - Ramona Marasco
- Biological and Environmental Sciences and Engineering Division, King Abdullah University of Science and Technology, Thuwal, Saudi Arabia
| | - Marco Fusi
- Biological and Environmental Sciences and Engineering Division, King Abdullah University of Science and Technology, Thuwal, Saudi Arabia.,Centre for Conservation and Restoration Science, Edinburgh Napier University, Edinburgh, UK
| | - Barbara Scaglia
- Department of Agricultural and Environmental Sciences-Production, Landscape, Agroenergy-Gruppo Ricicla Lab, University of Milan, Milan, Italy
| | - Florence Schubotz
- MARUM, Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
| | - Francesca Mapelli
- Department of Food, Environmental and Nutritional Sciences, University of Milan, Milan, Italy
| | - Sonia Ciccazzo
- Faculty of Science and Technology, Free University of Bolzano, Bolzano, Italy
| | - Lorenzo Brusetti
- Faculty of Science and Technology, Free University of Bolzano, Bolzano, Italy
| | - Luca Trombino
- Department of Earth Sciences 'Ardito Desio', University of Milan, Milan, Italy
| | - Fulvia Tambone
- Department of Agricultural and Environmental Sciences-Production, Landscape, Agroenergy-Gruppo Ricicla Lab, University of Milan, Milan, Italy
| | - Fabrizio Adani
- Department of Agricultural and Environmental Sciences-Production, Landscape, Agroenergy-Gruppo Ricicla Lab, University of Milan, Milan, Italy
| | - Sara Borin
- Department of Food, Environmental and Nutritional Sciences, University of Milan, Milan, Italy
| | - Daniele Daffonchio
- Biological and Environmental Sciences and Engineering Division, King Abdullah University of Science and Technology, Thuwal, Saudi Arabia
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15
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Soil Formation and Mass Redistribution during the Holocene Using Meteoric 10Be, Soil Chemistry and Mineralogy. GEOSCIENCES 2022. [DOI: 10.3390/geosciences12020099] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
Soil development and erosion are important and opposing processes in the evolution of high-mountainous landscapes, though their dynamics are not fully understood. We compared soil development between a calcareous and a siliceous chronosequence in the central Swiss Alps at high altitudes, which both cover soil formation over the Holocene. We calculated element mass balances, long-term erosion rates based on meteoric 10Be and we determined the rates of soil formation. We also analyzed the shifts in the mineralogical composition, weathering indices, the particle size distribution, carbon stocks and oxalate extractable Fe, Al, and Mn. The siliceous soils had high chemical weathering rates at the early stage of soil formation that strongly decreased after a few millennia. The development of calcareous soil was characterized by high carbonate losses and a shift to finer soil texture. Soil erosion hampered the upbuilding of soil horizons in the early stages of soil development, which led to a delay in soil and vegetation development. This study shows how soil formation drivers change over time. In the early stages of soil development, the parent material predominantly drives soil formation while at later stages the vegetation becomes more dominant as it influences surface stability, hydrological pathways, and chemical weathering that determine water drainage and retention.
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16
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Ficetola GF, Marta S, Guerrieri A, Gobbi M, Ambrosini R, Fontaneto D, Zerboni A, Poulenard J, Caccianiga M, Thuiller W. Dynamics of Ecological Communities Following Current Retreat of Glaciers. ANNUAL REVIEW OF ECOLOGY, EVOLUTION, AND SYSTEMATICS 2021. [DOI: 10.1146/annurev-ecolsys-010521-040017] [Citation(s) in RCA: 10] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Abstract
Glaciers are retreating globally, and the resulting ice-free areas provide an experimental system for understanding species colonization patterns, community formation, and dynamics. The last several years have seen crucial advances in our understanding of biotic colonization after glacier retreats, resulting from the integration of methodological innovations and ecological theories. Recent empirical studies have demonstrated how multiple factors can speed up or slow down the velocity of colonization and have helped scientists develop theoretical models that describe spatiotemporalchanges in community structure. There is a growing awareness of how different processes (e.g., time since glacier retreat, onset or interruption of surface processes, abiotic factors, dispersal, biotic interactions) interact to shape community formation and, ultimately, their functional structure through succession. Here, we examine how these studies address key theoretical questions about community dynamics and show how classical approaches are increasingly being combined with environmental DNA metabarcoding and functional trait analysis to document the formation of multitrophic communities, revolutionizing our understanding of the biotic processes that occur following glacier retreat.
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Affiliation(s)
- Gentile Francesco Ficetola
- Department of Environmental Science and Policy, Università degli Studi di Milano, I-20133 Milano, Italy
- Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, LECA, Laboratoire d'Ecologie Alpine, F-38000, Grenoble, France
| | - Silvio Marta
- Department of Environmental Science and Policy, Università degli Studi di Milano, I-20133 Milano, Italy
| | - Alessia Guerrieri
- Department of Environmental Science and Policy, Università degli Studi di Milano, I-20133 Milano, Italy
| | - Mauro Gobbi
- Section of Invertebrate Zoology and Hydrobiology, MUSE-Science Museum, I-38122 Trento, Italy
| | - Roberto Ambrosini
- Department of Environmental Science and Policy, Università degli Studi di Milano, I-20133 Milano, Italy
| | - Diego Fontaneto
- Molecular Ecology Group, Water Research Institute (IRSA), Italian National Research Council (CNR), I-28922 Verbania Pallanza, Italy
| | - Andrea Zerboni
- Dipartimento di Scienze della Terra “A. Desio,” Università degli Studi di Milano, I-20133 Milano, Italy
| | - Jerome Poulenard
- Laboratory of Environments, Dynamics, and Mountain Territories (EDYTEM), Université Savoie Mont Blanc, Université Grenoble Alpes, CNRS, F‐73000 Chambéry, France
| | - Marco Caccianiga
- Department of Biosciences, Università degli Studi di Milano, I-20133 Milano, Italy
| | - Wilfried Thuiller
- Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, LECA, Laboratoire d'Ecologie Alpine, F-38000, Grenoble, France
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17
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Abstract
Most of the world’s mountain glaciers have been retreating for more than a century in response to climate change. Glacier retreat is evident on all continents, and the rate of retreat has accelerated during recent decades. Accurate, spatially explicit information on the position of glacier margins over time is useful for analyzing patterns of glacier retreat and measuring reductions in glacier surface area. This information is also essential for evaluating how mountain ecosystems are evolving due to climate warming and the attendant glacier retreat. Here, we present a non-comprehensive spatially explicit dataset showing multiple positions of glacier fronts since the Little Ice Age (LIA) maxima, including many data from the pre-satellite era. The dataset is based on multiple historical archival records including topographical maps; repeated photographs, paintings, and aerial or satellite images with a supplement of geochronology; and own field data. We provide ESRI shapefiles showing 728 past positions of 94 glacier fronts from all continents, except Antarctica, covering the period between the Little Ice Age maxima and the present. On average, the time series span the past 190 years. From 2 to 46 past positions per glacier are depicted (on average: 7.8).
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