Pub Date : 2024-12-28DOI: 10.1038/s43247-024-01972-w
Aaron Micallef, Giovanni Barreca, Christian Hübscher, Angelo Camerlenghi, Paul Carling, Jose Maria Abril Hernandez, Raúl Periáñez, Daniel Garcia-Castellanos, Jonathan Ford, Benedikt Haimerl, Matthias Hartge, Jonas Preine, Antonio Caruso
One debated scenario for the termination of the Messinian salinity crisis 5.33 million years ago is cataclysmic refilling of the Mediterranean Sea through the Zanclean megaflood. Here we present a clear line of onshore-to-offshore evidence for this megaflood spilling over a shallow-water marine corridor in south-east Sicily into the nearby subaqueous Noto Canyon: (i) >300 asymmetric and streamlined erosional ridges aligned with the megaflood direction, (ii) poorly-sorted breccia deposited between the Messinian and Lower Zanclean Trubi Formations, (iii) soft-sediment deformation structures and clastic injections in the breccia and underlying units, and (iv) a 20 kilometre wide erosional shelf channel connecting the ridges with Noto Canyon. Numerical modelling results support the modulation of flow velocity and direction by the excavation of the channel and Noto Canyon. Our findings demonstrate that the Messinian salinity crisis was terminated through a cataclysmic flood, which implies pronounced Mediterranean sea-level drawdown prior to the flooding. The Zanclean megaflood poured water from the western to the eastern Mediterranean basin through a shallow marine corridor in south-eastern Sicily, ending the isolation of the Mediterranean Sea from the global oceans about 5.3 million years ago, according to onshore-offshore geological data from southern Sicily and numerical modelling.
{"title":"Land-to-sea indicators of the Zanclean megaflood","authors":"Aaron Micallef, Giovanni Barreca, Christian Hübscher, Angelo Camerlenghi, Paul Carling, Jose Maria Abril Hernandez, Raúl Periáñez, Daniel Garcia-Castellanos, Jonathan Ford, Benedikt Haimerl, Matthias Hartge, Jonas Preine, Antonio Caruso","doi":"10.1038/s43247-024-01972-w","DOIUrl":"10.1038/s43247-024-01972-w","url":null,"abstract":"One debated scenario for the termination of the Messinian salinity crisis 5.33 million years ago is cataclysmic refilling of the Mediterranean Sea through the Zanclean megaflood. Here we present a clear line of onshore-to-offshore evidence for this megaflood spilling over a shallow-water marine corridor in south-east Sicily into the nearby subaqueous Noto Canyon: (i) >300 asymmetric and streamlined erosional ridges aligned with the megaflood direction, (ii) poorly-sorted breccia deposited between the Messinian and Lower Zanclean Trubi Formations, (iii) soft-sediment deformation structures and clastic injections in the breccia and underlying units, and (iv) a 20 kilometre wide erosional shelf channel connecting the ridges with Noto Canyon. Numerical modelling results support the modulation of flow velocity and direction by the excavation of the channel and Noto Canyon. Our findings demonstrate that the Messinian salinity crisis was terminated through a cataclysmic flood, which implies pronounced Mediterranean sea-level drawdown prior to the flooding. The Zanclean megaflood poured water from the western to the eastern Mediterranean basin through a shallow marine corridor in south-eastern Sicily, ending the isolation of the Mediterranean Sea from the global oceans about 5.3 million years ago, according to onshore-offshore geological data from southern Sicily and numerical modelling.","PeriodicalId":10530,"journal":{"name":"Communications Earth & Environment","volume":" ","pages":"1-11"},"PeriodicalIF":8.1,"publicationDate":"2024-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.nature.com/articles/s43247-024-01972-w.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142906131","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-12-27DOI: 10.1038/s43247-024-01954-y
Sumudu Rajakaruna, Ghiwa Makke, Nathalia Graf Grachet, Christian Ayala-Ortiz, John Bouranis, David W. Hoyt, Jason Toyoda, Elizabeth H. Denis, James J. Moran, Tianze Song, Xiaoxu Sun, Elizabeth K. Eder, Allison R. Wong, Rosalie Chu, Heino Heyman, Max Kolton, Jeffrey P. Chanton, Rachel M. Wilson, Joel Kostka, Malak M. Tfaily
Peatlands store vast amounts of carbon, with deep peat carbon remaining stable due to limited thermodynamic energy and transport. However, climate change-induced increases in labile carbon inputs could destabilize these stores. Here, we combined DNA stable isotope probing with stable isotope-assisted metabolomics employing a multi-platform approach to investigate microbial dynamics driving deep peat carbon degradation upon labile carbon (e.g., glucose) amendment. Our findings highlight the vulnerability of deep peat carbon, as glucose addition triggers the breakdown of older organic matter. By uniquely integrating these techniques, we identified active glucose metabolizers to specific microbial populations and mapped carbon flow through microbial networks, elucidating their role in priming recalcitrant carbon mineralization. This multi-omics approach offers crucial insights into how changing resources reshape the peatland microbiome, enhancing our understanding of deep carbon processing, and refining model parameterization to predict microbial responses and carbon cycle feedbacks under global change pressures. Glucose addition to peatland soils promotes decomposition of older buried carbon through enhanced microbial activity, according to DNA analysis and isotope labelling of peatland soil.
{"title":"Adding labile carbon to peatland soils triggers deep carbon breakdown","authors":"Sumudu Rajakaruna, Ghiwa Makke, Nathalia Graf Grachet, Christian Ayala-Ortiz, John Bouranis, David W. Hoyt, Jason Toyoda, Elizabeth H. Denis, James J. Moran, Tianze Song, Xiaoxu Sun, Elizabeth K. Eder, Allison R. Wong, Rosalie Chu, Heino Heyman, Max Kolton, Jeffrey P. Chanton, Rachel M. Wilson, Joel Kostka, Malak M. Tfaily","doi":"10.1038/s43247-024-01954-y","DOIUrl":"10.1038/s43247-024-01954-y","url":null,"abstract":"Peatlands store vast amounts of carbon, with deep peat carbon remaining stable due to limited thermodynamic energy and transport. However, climate change-induced increases in labile carbon inputs could destabilize these stores. Here, we combined DNA stable isotope probing with stable isotope-assisted metabolomics employing a multi-platform approach to investigate microbial dynamics driving deep peat carbon degradation upon labile carbon (e.g., glucose) amendment. Our findings highlight the vulnerability of deep peat carbon, as glucose addition triggers the breakdown of older organic matter. By uniquely integrating these techniques, we identified active glucose metabolizers to specific microbial populations and mapped carbon flow through microbial networks, elucidating their role in priming recalcitrant carbon mineralization. This multi-omics approach offers crucial insights into how changing resources reshape the peatland microbiome, enhancing our understanding of deep carbon processing, and refining model parameterization to predict microbial responses and carbon cycle feedbacks under global change pressures. Glucose addition to peatland soils promotes decomposition of older buried carbon through enhanced microbial activity, according to DNA analysis and isotope labelling of peatland soil.","PeriodicalId":10530,"journal":{"name":"Communications Earth & Environment","volume":" ","pages":"1-14"},"PeriodicalIF":8.1,"publicationDate":"2024-12-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.nature.com/articles/s43247-024-01954-y.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142906156","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-12-26DOI: 10.1038/s43247-024-01968-6
Maaike F. M. Weerdesteijn, Clinton P. Conrad
Around the periphery of the Greenland ice sheet, satellite-based observations of ground uplift record Earth’s response to past and recent unloading of Greenland’s ice mass. On the southeast coast, near the Kangerlussuaq glacier, rapid uplift exceeding 12 mm/yr cannot be explained using current layered Earth deformation models. Here we find that 3D models with a weakened Earth structure, consistent with the passage of Greenland over the Iceland plume, can explain the rapid uplift of Southeast Greenland. This uplift is dominated by a viscous response that is accelerated by the low viscosities of the hot plume track. Recent mass loss, occurring during the last millennium and especially within the past few decades, drives most of the uplift. Holocene indicators recorded similarly rapid uplift following deglaciation that ended the last ice age. Such rapid uplift, occurring beneath marine terminating glaciers, can affect the future stability of entire ice catchment areas and will become increasingly important in the near future as deglaciation accelerates. Unusually rapid uplift of Southeast Greenland is explained as a viscous response to recent deglaciation occurring above mantle weakened by the Iceland plume, according to 3D modelling with a hot plume track that crosses Greenland’s southeast coast.
{"title":"Recent ice melt above a mantle plume track is accelerating the uplift of Southeast Greenland","authors":"Maaike F. M. Weerdesteijn, Clinton P. Conrad","doi":"10.1038/s43247-024-01968-6","DOIUrl":"10.1038/s43247-024-01968-6","url":null,"abstract":"Around the periphery of the Greenland ice sheet, satellite-based observations of ground uplift record Earth’s response to past and recent unloading of Greenland’s ice mass. On the southeast coast, near the Kangerlussuaq glacier, rapid uplift exceeding 12 mm/yr cannot be explained using current layered Earth deformation models. Here we find that 3D models with a weakened Earth structure, consistent with the passage of Greenland over the Iceland plume, can explain the rapid uplift of Southeast Greenland. This uplift is dominated by a viscous response that is accelerated by the low viscosities of the hot plume track. Recent mass loss, occurring during the last millennium and especially within the past few decades, drives most of the uplift. Holocene indicators recorded similarly rapid uplift following deglaciation that ended the last ice age. Such rapid uplift, occurring beneath marine terminating glaciers, can affect the future stability of entire ice catchment areas and will become increasingly important in the near future as deglaciation accelerates. Unusually rapid uplift of Southeast Greenland is explained as a viscous response to recent deglaciation occurring above mantle weakened by the Iceland plume, according to 3D modelling with a hot plume track that crosses Greenland’s southeast coast.","PeriodicalId":10530,"journal":{"name":"Communications Earth & Environment","volume":" ","pages":"1-15"},"PeriodicalIF":8.1,"publicationDate":"2024-12-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.nature.com/articles/s43247-024-01968-6.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142906159","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-12-24DOI: 10.1038/s43247-024-01959-7
Sagar P. Parajuli, Trent Biggs, Fernando de Sales, Miguel Angel Zavala Perez, Cenlin He, Charles Jones, Callum Thompson, Nicolas Lopez Galvez, Haley Ciborowski, Tiago Quintino, Claudia Di Napoli, Aliasghar Montazar, Tayebeh Hosseini Yazdi, Monica Soucier
Farmworkers, the frontline workers of our food system, are often exposed to heat stress that is likely to increase in frequency and severity due to climate change. Irrigation can either alleviate or exacerbate heat stress, quantification of which is crucial in intensely irrigated agricultural lands such as the Imperial Valley in southern California. We investigate the impact of irrigation on wet bulb globe temperature (WBGT), a key indicator of heat exposure in humans, using a validated high-resolution Weather Research and Forecasting (WRF) regional climate model, during day and night and in different seasons. We find that irrigation reduces WBGT by 0.3–1.3 °C during the daytime in summer due to strong evaporative cooling. However, during the summer nights, irrigation increases WBGT by 0.4–1.3 °C, when a large increase in humidity sufficiently raises the wet-bulb temperature. Urban and fallow areas adjacent to cropped fields also experience increased heat stress due to moisture advection from irrigated areas. Our results can inform heat-related policies in agricultural regions of California and elsewhere. In the Imperial Valley of California, irrigation of agricultural fields in summer decreases farmworker’s heat stress in the daytime but increases it at night, according to an analysis that uses high-resolution data from a regional climate model.
{"title":"Impact of irrigation on farmworker’s heat stress in California differs by season and during the day and night","authors":"Sagar P. Parajuli, Trent Biggs, Fernando de Sales, Miguel Angel Zavala Perez, Cenlin He, Charles Jones, Callum Thompson, Nicolas Lopez Galvez, Haley Ciborowski, Tiago Quintino, Claudia Di Napoli, Aliasghar Montazar, Tayebeh Hosseini Yazdi, Monica Soucier","doi":"10.1038/s43247-024-01959-7","DOIUrl":"10.1038/s43247-024-01959-7","url":null,"abstract":"Farmworkers, the frontline workers of our food system, are often exposed to heat stress that is likely to increase in frequency and severity due to climate change. Irrigation can either alleviate or exacerbate heat stress, quantification of which is crucial in intensely irrigated agricultural lands such as the Imperial Valley in southern California. We investigate the impact of irrigation on wet bulb globe temperature (WBGT), a key indicator of heat exposure in humans, using a validated high-resolution Weather Research and Forecasting (WRF) regional climate model, during day and night and in different seasons. We find that irrigation reduces WBGT by 0.3–1.3 °C during the daytime in summer due to strong evaporative cooling. However, during the summer nights, irrigation increases WBGT by 0.4–1.3 °C, when a large increase in humidity sufficiently raises the wet-bulb temperature. Urban and fallow areas adjacent to cropped fields also experience increased heat stress due to moisture advection from irrigated areas. Our results can inform heat-related policies in agricultural regions of California and elsewhere. In the Imperial Valley of California, irrigation of agricultural fields in summer decreases farmworker’s heat stress in the daytime but increases it at night, according to an analysis that uses high-resolution data from a regional climate model.","PeriodicalId":10530,"journal":{"name":"Communications Earth & Environment","volume":" ","pages":"1-16"},"PeriodicalIF":8.1,"publicationDate":"2024-12-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.nature.com/articles/s43247-024-01959-7.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142880583","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-12-24DOI: 10.1038/s43247-024-01928-0
Mehebub Sahana, Md Kutubuddin Dhali, Sarah Lindley
Anthropogenic pressures, climate change, and hydro-politics pose significant risks for sustainable transboundary river basin management. We reviewed 4237 publications using machine learning and conducted a desk review of 325 publications, analyzing 4713 case studies across 286 basins. Our objectives were to: assess major perspectives and key research themes; analyse how they vary based on basin size, location, runoff, water withdrawal, discharge, and consumption; and reflect on implications for sustainable basin management. Findings show that the volume of research in the global south is disproportionately small compared to basin population size, water withdrawals and water consumption. Moreover, research is predominantly led by global north institutions, shaping study themes and locations. While research in the global south focuses on hydro-politics and natural hazards, the global north emphasizes landscape ecology and governance. These insights highlight the need for more comprehensive assessments in the global south to support sustainable management of transboundary river basins. The volume of research on transboundary rivers and management in the global south is disproportionately small compared to river basin population size, water withdrawals, and consumption, according to an analysis of 4713 case studies using machine learning and desk review.
{"title":"Global disparities in transboundary river research have implications for sustainable management","authors":"Mehebub Sahana, Md Kutubuddin Dhali, Sarah Lindley","doi":"10.1038/s43247-024-01928-0","DOIUrl":"10.1038/s43247-024-01928-0","url":null,"abstract":"Anthropogenic pressures, climate change, and hydro-politics pose significant risks for sustainable transboundary river basin management. We reviewed 4237 publications using machine learning and conducted a desk review of 325 publications, analyzing 4713 case studies across 286 basins. Our objectives were to: assess major perspectives and key research themes; analyse how they vary based on basin size, location, runoff, water withdrawal, discharge, and consumption; and reflect on implications for sustainable basin management. Findings show that the volume of research in the global south is disproportionately small compared to basin population size, water withdrawals and water consumption. Moreover, research is predominantly led by global north institutions, shaping study themes and locations. While research in the global south focuses on hydro-politics and natural hazards, the global north emphasizes landscape ecology and governance. These insights highlight the need for more comprehensive assessments in the global south to support sustainable management of transboundary river basins. The volume of research on transboundary rivers and management in the global south is disproportionately small compared to river basin population size, water withdrawals, and consumption, according to an analysis of 4713 case studies using machine learning and desk review.","PeriodicalId":10530,"journal":{"name":"Communications Earth & Environment","volume":" ","pages":"1-17"},"PeriodicalIF":8.1,"publicationDate":"2024-12-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.nature.com/articles/s43247-024-01928-0.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142880571","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-12-23DOI: 10.1038/s43247-024-01971-x
Ding-Yi Xiong, Xiao-Lei Wang, Axel Hofmann, Weiqiang Li, Rong-Qing Zhang, Teimoor Nazari-Dehkordi, Yue Guan, Shi-Chao An
Formation of granite-hosted tin deposits reflects the differentiation and maturation of continental crust. While rare in Earth’s early continental crust, the eastern Kaapvaal Craton in southern Africa may harbor the oldest known tin-bearing granites. Here we present a perspective of early continental evolution from the study of Archean detrital cassiterite from the volcano-sedimentary continental cover succession of the Dominion Group of the western Kaapvaal Craton. The cassiterites yield a concordia age of 3084.7 ± 2.3 million-year-old, representing the oldest detrital cassiterite ever found. They are enriched in hafnium, zirconium, niobium, and tantalum, depleted in tungsten, and have overall consistent δ18O values (mostly 3‒5‰) but heterogeneous δ122/118Sn values (−0.59 to 0.79‰). They likely originated from erosion of peraluminous granites, forming immediate basement of the Dominion Group. The occurrence of ~3.08 billion-year-old detrital cassiterite suggests widespread tin mineralization in the granites, the intrusion of which led to stabilization of the Kaapvaal craton. A detrital cassiterite found in the Kaapvaal Craton, South Africa, implies widespread tin mineralization and stabilization of granitic cratons approximately 3.08 billion years ago, as shown by U-Pb geochronology, trace element and oxygen and tin isotopes.
{"title":"3.08 billion-year-old crustal differentiation constrained by Sn and O isotopes of detrital cassiterite","authors":"Ding-Yi Xiong, Xiao-Lei Wang, Axel Hofmann, Weiqiang Li, Rong-Qing Zhang, Teimoor Nazari-Dehkordi, Yue Guan, Shi-Chao An","doi":"10.1038/s43247-024-01971-x","DOIUrl":"10.1038/s43247-024-01971-x","url":null,"abstract":"Formation of granite-hosted tin deposits reflects the differentiation and maturation of continental crust. While rare in Earth’s early continental crust, the eastern Kaapvaal Craton in southern Africa may harbor the oldest known tin-bearing granites. Here we present a perspective of early continental evolution from the study of Archean detrital cassiterite from the volcano-sedimentary continental cover succession of the Dominion Group of the western Kaapvaal Craton. The cassiterites yield a concordia age of 3084.7 ± 2.3 million-year-old, representing the oldest detrital cassiterite ever found. They are enriched in hafnium, zirconium, niobium, and tantalum, depleted in tungsten, and have overall consistent δ18O values (mostly 3‒5‰) but heterogeneous δ122/118Sn values (−0.59 to 0.79‰). They likely originated from erosion of peraluminous granites, forming immediate basement of the Dominion Group. The occurrence of ~3.08 billion-year-old detrital cassiterite suggests widespread tin mineralization in the granites, the intrusion of which led to stabilization of the Kaapvaal craton. A detrital cassiterite found in the Kaapvaal Craton, South Africa, implies widespread tin mineralization and stabilization of granitic cratons approximately 3.08 billion years ago, as shown by U-Pb geochronology, trace element and oxygen and tin isotopes.","PeriodicalId":10530,"journal":{"name":"Communications Earth & Environment","volume":" ","pages":"1-9"},"PeriodicalIF":8.1,"publicationDate":"2024-12-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.nature.com/articles/s43247-024-01971-x.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142870543","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Inland lakes are a crucial source of greenhouse gases, such as carbon dioxide, methane and nitrous oxide. The interconnected river-lake systems feature multiple lake regions, wherein numerous rivers interconnect various lake regions. Their intricate hydrological conditions and interactions distinguish them from conventional lakes, which typically have a single and relatively static water body. However, the greenhouse gas emission characteristics, as well as the driving forces of the interconnected river-lake systems, are still under-researched. Here, we carried out bi-seasonal in situ surveys across a typical interconnected river-lake system, Dongting Lake, along with a meta-analysis derived from 168 lakes spanning six continents, to elucidate this issue. We found that interconnected river-lake systems exhibit a unique temporal variation in carbon dioxide and nitrous oxide fluxes, with positive fluxes during the wet season but transitioning to sinks during the dry season. Greenhouse gas fluxes in conventional stable lakes are frequently correlated with abiotic factors, such as hydro-climatological conditions and trophic status. While in Dongting Lake, specific microbial species that are important to the cycling of macronutrients and other less common nutrients, alongside microbial predatory behaviour, can better predict greenhouse gas fluxes. Our study highlights the importance of biotic predictors in prospective greenhouse gases flux estimates. River-lake ecosystems act as carbon dioxide and nitrous oxide sources in the wet season and sinks in the dry season, according to an analysis of greenhouse gas emissions from Dongting Lake, China, combined with a global-scale meta-analysis.
{"title":"River-lake ecosystems exhibit a strong seasonal cycle of greenhouse gas emissions","authors":"Shijie Wang, Shanghua Wu, Yuzhu Dong, Xianglong Li, Yaxin Wang, Yijing Li, Ying Zhu, Jiahui Deng, Xuliang Zhuang","doi":"10.1038/s43247-024-01912-8","DOIUrl":"10.1038/s43247-024-01912-8","url":null,"abstract":"Inland lakes are a crucial source of greenhouse gases, such as carbon dioxide, methane and nitrous oxide. The interconnected river-lake systems feature multiple lake regions, wherein numerous rivers interconnect various lake regions. Their intricate hydrological conditions and interactions distinguish them from conventional lakes, which typically have a single and relatively static water body. However, the greenhouse gas emission characteristics, as well as the driving forces of the interconnected river-lake systems, are still under-researched. Here, we carried out bi-seasonal in situ surveys across a typical interconnected river-lake system, Dongting Lake, along with a meta-analysis derived from 168 lakes spanning six continents, to elucidate this issue. We found that interconnected river-lake systems exhibit a unique temporal variation in carbon dioxide and nitrous oxide fluxes, with positive fluxes during the wet season but transitioning to sinks during the dry season. Greenhouse gas fluxes in conventional stable lakes are frequently correlated with abiotic factors, such as hydro-climatological conditions and trophic status. While in Dongting Lake, specific microbial species that are important to the cycling of macronutrients and other less common nutrients, alongside microbial predatory behaviour, can better predict greenhouse gas fluxes. Our study highlights the importance of biotic predictors in prospective greenhouse gases flux estimates. River-lake ecosystems act as carbon dioxide and nitrous oxide sources in the wet season and sinks in the dry season, according to an analysis of greenhouse gas emissions from Dongting Lake, China, combined with a global-scale meta-analysis.","PeriodicalId":10530,"journal":{"name":"Communications Earth & Environment","volume":" ","pages":"1-13"},"PeriodicalIF":8.1,"publicationDate":"2024-12-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.nature.com/articles/s43247-024-01912-8.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142870497","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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