The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon
- Autores
- Cotton, Jennifer M.; Ghosh, Adit; Hyland, Ethan; Hauswirth, Scott; Littleton, Shelby; Azmi, Iffat; Insel, Nadja; Raigemborn, María Sol; Tineo, David
- Año de publicación
- 2023
- Idioma
- inglés
- Tipo de recurso
- documento de conferencia
- Estado
- versión publicada
- Descripción
- The expansion of C4 grasses is one of the most dramatic ecological changes in the past 65 million years. Beginning in the late Miocene (~7 million years ago), these tropical and subtropical grasses began to spread and now cover roughly 25% of the Earth's surface. C4 grasses include economically important crops such as corn, sugarcane and sorghum, but the environmental conditions that drove this global expansion are poorly understood. In this study, we aim to determine the drivers of C4 grass expansion in South America. We hypothesize that this expansion was driven by the strengthening of the South American Summer Monsoon (SASM), which occurred as a result of regional climatic change due to local tectonic and global climatic changes. Using carbon isotopes of bulk organic matter preserved in paleosols, we reconstruct the abundance of C4 grasses across 7 sites in Argentina to assess the timing of this ecological transition in South America. We pair this C4 grass reconstruction with phytolith and biomarker analysis to gain a more detailed perspective of vegetation and fire history, and we use soil geochemistry proxies to assess changes in hydroclimate across the region from the late Miocene-Pliocene. We find that in the absence of temperature and atmospheric CO2 changes, hydrologic change is likely the driver of C4 grass abundances in the Miocene. In far northwest Argentina, our data suggests that increased seasonality brought about by the intensification of the South American Monsoon drove the expansion of C4 grasses, at least in the more humid regions. These results are supported by Community Earth System Model simulations that suggest an increase in summer precipitation along the eastern foothills of the Andes in Northern Argentina between 8 and 3Ma. Our data does not show a correlation between fire frequency and C4 grass abundance in Argentina, unlike in the Siwaliks of South Asia. We also note that we only find moderate to high abundances of C4 grasses in areas where proxy-based precipitation estimates exceed ~500mm/yr. We also do not observe C4 grasses at sites with modern elevations higher than ~3,000 feet or behind rain shadows, showing that tectonically-driven climate changes are important controls on the distribution and spread of C4 grasses. This work will allow us to better predict changes to modern grasslands in the future.
Fil: Cotton, Jennifer M.. Departament Of Geological Sciences ; College Of Science And Mathematics ; California State University Northridge;
Fil: Ghosh, Adit. University of Southern California; Estados Unidos
Fil: Hyland, Ethan. North Carolina State University; Estados Unidos
Fil: Hauswirth, Scott. Departament Of Geological Sciences ; College Of Science And Mathematics ; California State University Northridge;
Fil: Littleton, Shelby. Departament Of Geological Sciences ; College Of Science And Mathematics ; California State University Northridge;
Fil: Azmi, Iffat. North Carolina State University; Estados Unidos
Fil: Insel, Nadja. Northeastern Illinois University (northeastern Illinois);
Fil: Raigemborn, María Sol. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Tineo, David. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
73rd Annual Meeting of the Rocky Mountain Section
Fort Collins
Estados Unidos
The Geological Society of America - Materia
-
C4 GRASSES
SOUTH AMERICA
GRASSLAND TRANSITION
SOUTH AMERICAN SUMMER MONSOON - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/256564
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The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoonCotton, Jennifer M.Ghosh, AditHyland, EthanHauswirth, ScottLittleton, ShelbyAzmi, IffatInsel, NadjaRaigemborn, María SolTineo, DavidC4 GRASSESSOUTH AMERICAGRASSLAND TRANSITIONSOUTH AMERICAN SUMMER MONSOONhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The expansion of C4 grasses is one of the most dramatic ecological changes in the past 65 million years. Beginning in the late Miocene (~7 million years ago), these tropical and subtropical grasses began to spread and now cover roughly 25% of the Earth's surface. C4 grasses include economically important crops such as corn, sugarcane and sorghum, but the environmental conditions that drove this global expansion are poorly understood. In this study, we aim to determine the drivers of C4 grass expansion in South America. We hypothesize that this expansion was driven by the strengthening of the South American Summer Monsoon (SASM), which occurred as a result of regional climatic change due to local tectonic and global climatic changes. Using carbon isotopes of bulk organic matter preserved in paleosols, we reconstruct the abundance of C4 grasses across 7 sites in Argentina to assess the timing of this ecological transition in South America. We pair this C4 grass reconstruction with phytolith and biomarker analysis to gain a more detailed perspective of vegetation and fire history, and we use soil geochemistry proxies to assess changes in hydroclimate across the region from the late Miocene-Pliocene. We find that in the absence of temperature and atmospheric CO2 changes, hydrologic change is likely the driver of C4 grass abundances in the Miocene. In far northwest Argentina, our data suggests that increased seasonality brought about by the intensification of the South American Monsoon drove the expansion of C4 grasses, at least in the more humid regions. These results are supported by Community Earth System Model simulations that suggest an increase in summer precipitation along the eastern foothills of the Andes in Northern Argentina between 8 and 3Ma. Our data does not show a correlation between fire frequency and C4 grass abundance in Argentina, unlike in the Siwaliks of South Asia. We also note that we only find moderate to high abundances of C4 grasses in areas where proxy-based precipitation estimates exceed ~500mm/yr. We also do not observe C4 grasses at sites with modern elevations higher than ~3,000 feet or behind rain shadows, showing that tectonically-driven climate changes are important controls on the distribution and spread of C4 grasses. This work will allow us to better predict changes to modern grasslands in the future.Fil: Cotton, Jennifer M.. Departament Of Geological Sciences ; College Of Science And Mathematics ; California State University Northridge;Fil: Ghosh, Adit. University of Southern California; Estados UnidosFil: Hyland, Ethan. North Carolina State University; Estados UnidosFil: Hauswirth, Scott. Departament Of Geological Sciences ; College Of Science And Mathematics ; California State University Northridge;Fil: Littleton, Shelby. Departament Of Geological Sciences ; College Of Science And Mathematics ; California State University Northridge;Fil: Azmi, Iffat. North Carolina State University; Estados UnidosFil: Insel, Nadja. Northeastern Illinois University (northeastern Illinois);Fil: Raigemborn, María Sol. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Tineo, David. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina73rd Annual Meeting of the Rocky Mountain SectionFort CollinsEstados UnidosThe Geological Society of AmericaThe Geological Society of America2023info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectReuniónJournalhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/256564The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon; 73rd Annual Meeting of the Rocky Mountain Section; Fort Collins; Estados Unidos; 2023; 1-10016-7592CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1130/abs/2023RM-387979info:eu-repo/semantics/altIdentifier/url/https://gsa.confex.com/gsa/2023RM/meetingapp.cgi/Paper/387979Internacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:49:48Zoai:ri.conicet.gov.ar:11336/256564instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:49:48.632CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon |
title |
The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon |
spellingShingle |
The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon Cotton, Jennifer M. C4 GRASSES SOUTH AMERICA GRASSLAND TRANSITION SOUTH AMERICAN SUMMER MONSOON |
title_short |
The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon |
title_full |
The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon |
title_fullStr |
The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon |
title_full_unstemmed |
The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon |
title_sort |
The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon |
dc.creator.none.fl_str_mv |
Cotton, Jennifer M. Ghosh, Adit Hyland, Ethan Hauswirth, Scott Littleton, Shelby Azmi, Iffat Insel, Nadja Raigemborn, María Sol Tineo, David |
author |
Cotton, Jennifer M. |
author_facet |
Cotton, Jennifer M. Ghosh, Adit Hyland, Ethan Hauswirth, Scott Littleton, Shelby Azmi, Iffat Insel, Nadja Raigemborn, María Sol Tineo, David |
author_role |
author |
author2 |
Ghosh, Adit Hyland, Ethan Hauswirth, Scott Littleton, Shelby Azmi, Iffat Insel, Nadja Raigemborn, María Sol Tineo, David |
author2_role |
author author author author author author author author |
dc.subject.none.fl_str_mv |
C4 GRASSES SOUTH AMERICA GRASSLAND TRANSITION SOUTH AMERICAN SUMMER MONSOON |
topic |
C4 GRASSES SOUTH AMERICA GRASSLAND TRANSITION SOUTH AMERICAN SUMMER MONSOON |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The expansion of C4 grasses is one of the most dramatic ecological changes in the past 65 million years. Beginning in the late Miocene (~7 million years ago), these tropical and subtropical grasses began to spread and now cover roughly 25% of the Earth's surface. C4 grasses include economically important crops such as corn, sugarcane and sorghum, but the environmental conditions that drove this global expansion are poorly understood. In this study, we aim to determine the drivers of C4 grass expansion in South America. We hypothesize that this expansion was driven by the strengthening of the South American Summer Monsoon (SASM), which occurred as a result of regional climatic change due to local tectonic and global climatic changes. Using carbon isotopes of bulk organic matter preserved in paleosols, we reconstruct the abundance of C4 grasses across 7 sites in Argentina to assess the timing of this ecological transition in South America. We pair this C4 grass reconstruction with phytolith and biomarker analysis to gain a more detailed perspective of vegetation and fire history, and we use soil geochemistry proxies to assess changes in hydroclimate across the region from the late Miocene-Pliocene. We find that in the absence of temperature and atmospheric CO2 changes, hydrologic change is likely the driver of C4 grass abundances in the Miocene. In far northwest Argentina, our data suggests that increased seasonality brought about by the intensification of the South American Monsoon drove the expansion of C4 grasses, at least in the more humid regions. These results are supported by Community Earth System Model simulations that suggest an increase in summer precipitation along the eastern foothills of the Andes in Northern Argentina between 8 and 3Ma. Our data does not show a correlation between fire frequency and C4 grass abundance in Argentina, unlike in the Siwaliks of South Asia. We also note that we only find moderate to high abundances of C4 grasses in areas where proxy-based precipitation estimates exceed ~500mm/yr. We also do not observe C4 grasses at sites with modern elevations higher than ~3,000 feet or behind rain shadows, showing that tectonically-driven climate changes are important controls on the distribution and spread of C4 grasses. This work will allow us to better predict changes to modern grasslands in the future. Fil: Cotton, Jennifer M.. Departament Of Geological Sciences ; College Of Science And Mathematics ; California State University Northridge; Fil: Ghosh, Adit. University of Southern California; Estados Unidos Fil: Hyland, Ethan. North Carolina State University; Estados Unidos Fil: Hauswirth, Scott. Departament Of Geological Sciences ; College Of Science And Mathematics ; California State University Northridge; Fil: Littleton, Shelby. Departament Of Geological Sciences ; College Of Science And Mathematics ; California State University Northridge; Fil: Azmi, Iffat. North Carolina State University; Estados Unidos Fil: Insel, Nadja. Northeastern Illinois University (northeastern Illinois); Fil: Raigemborn, María Sol. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: Tineo, David. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina 73rd Annual Meeting of the Rocky Mountain Section Fort Collins Estados Unidos The Geological Society of America |
description |
The expansion of C4 grasses is one of the most dramatic ecological changes in the past 65 million years. Beginning in the late Miocene (~7 million years ago), these tropical and subtropical grasses began to spread and now cover roughly 25% of the Earth's surface. C4 grasses include economically important crops such as corn, sugarcane and sorghum, but the environmental conditions that drove this global expansion are poorly understood. In this study, we aim to determine the drivers of C4 grass expansion in South America. We hypothesize that this expansion was driven by the strengthening of the South American Summer Monsoon (SASM), which occurred as a result of regional climatic change due to local tectonic and global climatic changes. Using carbon isotopes of bulk organic matter preserved in paleosols, we reconstruct the abundance of C4 grasses across 7 sites in Argentina to assess the timing of this ecological transition in South America. We pair this C4 grass reconstruction with phytolith and biomarker analysis to gain a more detailed perspective of vegetation and fire history, and we use soil geochemistry proxies to assess changes in hydroclimate across the region from the late Miocene-Pliocene. We find that in the absence of temperature and atmospheric CO2 changes, hydrologic change is likely the driver of C4 grass abundances in the Miocene. In far northwest Argentina, our data suggests that increased seasonality brought about by the intensification of the South American Monsoon drove the expansion of C4 grasses, at least in the more humid regions. These results are supported by Community Earth System Model simulations that suggest an increase in summer precipitation along the eastern foothills of the Andes in Northern Argentina between 8 and 3Ma. Our data does not show a correlation between fire frequency and C4 grass abundance in Argentina, unlike in the Siwaliks of South Asia. We also note that we only find moderate to high abundances of C4 grasses in areas where proxy-based precipitation estimates exceed ~500mm/yr. We also do not observe C4 grasses at sites with modern elevations higher than ~3,000 feet or behind rain shadows, showing that tectonically-driven climate changes are important controls on the distribution and spread of C4 grasses. This work will allow us to better predict changes to modern grasslands in the future. |
publishDate |
2023 |
dc.date.none.fl_str_mv |
2023 |
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info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/conferenceObject Reunión Journal http://purl.org/coar/resource_type/c_5794 info:ar-repo/semantics/documentoDeConferencia |
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publishedVersion |
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conferenceObject |
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http://hdl.handle.net/11336/256564 The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon; 73rd Annual Meeting of the Rocky Mountain Section; Fort Collins; Estados Unidos; 2023; 1-1 0016-7592 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/256564 |
identifier_str_mv |
The rise of C4 grasses in South America: Linking grassland transition to the South American summer monsoon; 73rd Annual Meeting of the Rocky Mountain Section; Fort Collins; Estados Unidos; 2023; 1-1 0016-7592 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
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info:eu-repo/semantics/altIdentifier/doi/10.1130/abs/2023RM-387979 info:eu-repo/semantics/altIdentifier/url/https://gsa.confex.com/gsa/2023RM/meetingapp.cgi/Paper/387979 |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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Internacional |
dc.publisher.none.fl_str_mv |
The Geological Society of America |
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The Geological Society of America |
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reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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