Late Holocene climate: Natural or anthropogenic?
For more than a decade, scientists have argued about the warmth of the current interglaciation. Was the warmth of the preindustrial late Holocene natural in origin, the result of orbital changes that had not yet driven the system into a new glacial state? Or was it in considerable degree the result...
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| Autor*in: |
Ruddiman, W. F [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Rechteinformationen: |
Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Reviews of geophysics - Washington, DC : AGU, 1963, 54(2016), 1, Seite 93-118 |
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| Übergeordnetes Werk: |
volume:54 ; year:2016 ; number:1 ; pages:93-118 |
| Links: |
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| DOI / URN: |
10.1002/2015RG000503 |
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| 520 | |a For more than a decade, scientists have argued about the warmth of the current interglaciation. Was the warmth of the preindustrial late Holocene natural in origin, the result of orbital changes that had not yet driven the system into a new glacial state? Or was it in considerable degree the result of humans intervening in the climate system through greenhouse gas emissions from early agriculture? Here we summarize new evidence that moves this debate forward by testing both hypotheses. By comparing late Holocene responses to those that occurred during previous interglaciations (in section 2), we assess whether the late Holocene responses look different (and thus anthropogenic) or similar (and thus natural). This comparison reveals anomalous (anthropogenic) signals. In section 3, we review paleoecological and archaeological syntheses that provide ground truth evidence on early anthropogenic releases of greenhouse gases. The available data document large early anthropogenic emissions consistent with the anthropogenic ice core anomalies, but more information is needed to constrain their size. A final section compares natural and anthropogenic interpretations of the δ 13 C trend in ice core CO 2 . Holocene ice core and ocean sediment trends are anomalous compared to previous interglaciations Paleoecology and archaeology show that early farmers emitted large amounts of CO 2 and CH 4 Large early agricultural emissions are consistent with geochemical constraints | ||
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10.1002/2015RG000503 doi PQ20160430 (DE-627)OLC1972575422 (DE-599)GBVOLC1972575422 (PRQ)p954-4ee44dce2a685b1f7c67355d164c3bb0d0b8b0040aa01e98b091d55b6b4a3740 (KEY)0014642020160000054000100093lateholoceneclimatenaturaloranthropogenic DE-627 ger DE-627 rakwb eng 550 DNB Ruddiman, W. F verfasserin aut Late Holocene climate: Natural or anthropogenic? 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier For more than a decade, scientists have argued about the warmth of the current interglaciation. Was the warmth of the preindustrial late Holocene natural in origin, the result of orbital changes that had not yet driven the system into a new glacial state? Or was it in considerable degree the result of humans intervening in the climate system through greenhouse gas emissions from early agriculture? Here we summarize new evidence that moves this debate forward by testing both hypotheses. By comparing late Holocene responses to those that occurred during previous interglaciations (in section 2), we assess whether the late Holocene responses look different (and thus anthropogenic) or similar (and thus natural). This comparison reveals anomalous (anthropogenic) signals. In section 3, we review paleoecological and archaeological syntheses that provide ground truth evidence on early anthropogenic releases of greenhouse gases. The available data document large early anthropogenic emissions consistent with the anthropogenic ice core anomalies, but more information is needed to constrain their size. A final section compares natural and anthropogenic interpretations of the δ 13 C trend in ice core CO 2 . Holocene ice core and ocean sediment trends are anomalous compared to previous interglaciations Paleoecology and archaeology show that early farmers emitted large amounts of CO 2 and CH 4 Large early agricultural emissions are consistent with geochemical constraints Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. Holocene climate anthropogenic Emissions Fuller, D. Q oth Kutzbach, J. E oth Tzedakis, P. C oth Kaplan, J. O oth Ellis, E. C oth Vavrus, S. J oth Roberts, C. N oth Fyfe, R oth He, F oth Lemmen, C oth Woodbridge, J oth Enthalten in Reviews of geophysics Washington, DC : AGU, 1963 54(2016), 1, Seite 93-118 (DE-627)129509086 (DE-600)209852-0 (DE-576)014915685 0034-6853 nnns volume:54 year:2016 number:1 pages:93-118 http://dx.doi.org/10.1002/2015RG000503 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015RG000503/abstract http://search.proquest.com/docview/1782368040 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_62 GBV_ILN_601 AR 54 2016 1 93-118 |
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10.1002/2015RG000503 doi PQ20160430 (DE-627)OLC1972575422 (DE-599)GBVOLC1972575422 (PRQ)p954-4ee44dce2a685b1f7c67355d164c3bb0d0b8b0040aa01e98b091d55b6b4a3740 (KEY)0014642020160000054000100093lateholoceneclimatenaturaloranthropogenic DE-627 ger DE-627 rakwb eng 550 DNB Ruddiman, W. F verfasserin aut Late Holocene climate: Natural or anthropogenic? 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier For more than a decade, scientists have argued about the warmth of the current interglaciation. Was the warmth of the preindustrial late Holocene natural in origin, the result of orbital changes that had not yet driven the system into a new glacial state? Or was it in considerable degree the result of humans intervening in the climate system through greenhouse gas emissions from early agriculture? Here we summarize new evidence that moves this debate forward by testing both hypotheses. By comparing late Holocene responses to those that occurred during previous interglaciations (in section 2), we assess whether the late Holocene responses look different (and thus anthropogenic) or similar (and thus natural). This comparison reveals anomalous (anthropogenic) signals. In section 3, we review paleoecological and archaeological syntheses that provide ground truth evidence on early anthropogenic releases of greenhouse gases. The available data document large early anthropogenic emissions consistent with the anthropogenic ice core anomalies, but more information is needed to constrain their size. A final section compares natural and anthropogenic interpretations of the δ 13 C trend in ice core CO 2 . Holocene ice core and ocean sediment trends are anomalous compared to previous interglaciations Paleoecology and archaeology show that early farmers emitted large amounts of CO 2 and CH 4 Large early agricultural emissions are consistent with geochemical constraints Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. Holocene climate anthropogenic Emissions Fuller, D. Q oth Kutzbach, J. E oth Tzedakis, P. C oth Kaplan, J. O oth Ellis, E. C oth Vavrus, S. J oth Roberts, C. N oth Fyfe, R oth He, F oth Lemmen, C oth Woodbridge, J oth Enthalten in Reviews of geophysics Washington, DC : AGU, 1963 54(2016), 1, Seite 93-118 (DE-627)129509086 (DE-600)209852-0 (DE-576)014915685 0034-6853 nnns volume:54 year:2016 number:1 pages:93-118 http://dx.doi.org/10.1002/2015RG000503 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015RG000503/abstract http://search.proquest.com/docview/1782368040 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_62 GBV_ILN_601 AR 54 2016 1 93-118 |
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10.1002/2015RG000503 doi PQ20160430 (DE-627)OLC1972575422 (DE-599)GBVOLC1972575422 (PRQ)p954-4ee44dce2a685b1f7c67355d164c3bb0d0b8b0040aa01e98b091d55b6b4a3740 (KEY)0014642020160000054000100093lateholoceneclimatenaturaloranthropogenic DE-627 ger DE-627 rakwb eng 550 DNB Ruddiman, W. F verfasserin aut Late Holocene climate: Natural or anthropogenic? 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier For more than a decade, scientists have argued about the warmth of the current interglaciation. Was the warmth of the preindustrial late Holocene natural in origin, the result of orbital changes that had not yet driven the system into a new glacial state? Or was it in considerable degree the result of humans intervening in the climate system through greenhouse gas emissions from early agriculture? Here we summarize new evidence that moves this debate forward by testing both hypotheses. By comparing late Holocene responses to those that occurred during previous interglaciations (in section 2), we assess whether the late Holocene responses look different (and thus anthropogenic) or similar (and thus natural). This comparison reveals anomalous (anthropogenic) signals. In section 3, we review paleoecological and archaeological syntheses that provide ground truth evidence on early anthropogenic releases of greenhouse gases. The available data document large early anthropogenic emissions consistent with the anthropogenic ice core anomalies, but more information is needed to constrain their size. A final section compares natural and anthropogenic interpretations of the δ 13 C trend in ice core CO 2 . Holocene ice core and ocean sediment trends are anomalous compared to previous interglaciations Paleoecology and archaeology show that early farmers emitted large amounts of CO 2 and CH 4 Large early agricultural emissions are consistent with geochemical constraints Nutzungsrecht: © 2015. American Geophysical Union. All Rights Reserved. Holocene climate anthropogenic Emissions Fuller, D. Q oth Kutzbach, J. E oth Tzedakis, P. C oth Kaplan, J. O oth Ellis, E. C oth Vavrus, S. J oth Roberts, C. N oth Fyfe, R oth He, F oth Lemmen, C oth Woodbridge, J oth Enthalten in Reviews of geophysics Washington, DC : AGU, 1963 54(2016), 1, Seite 93-118 (DE-627)129509086 (DE-600)209852-0 (DE-576)014915685 0034-6853 nnns volume:54 year:2016 number:1 pages:93-118 http://dx.doi.org/10.1002/2015RG000503 Volltext http://onlinelibrary.wiley.com/doi/10.1002/2015RG000503/abstract http://search.proquest.com/docview/1782368040 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_62 GBV_ILN_601 AR 54 2016 1 93-118 |
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Late Holocene climate: Natural or anthropogenic? |
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Late Holocene climate: Natural or anthropogenic? |
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late holocene climate: natural or anthropogenic? |
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Late Holocene climate: Natural or anthropogenic? |
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For more than a decade, scientists have argued about the warmth of the current interglaciation. Was the warmth of the preindustrial late Holocene natural in origin, the result of orbital changes that had not yet driven the system into a new glacial state? Or was it in considerable degree the result of humans intervening in the climate system through greenhouse gas emissions from early agriculture? Here we summarize new evidence that moves this debate forward by testing both hypotheses. By comparing late Holocene responses to those that occurred during previous interglaciations (in section 2), we assess whether the late Holocene responses look different (and thus anthropogenic) or similar (and thus natural). This comparison reveals anomalous (anthropogenic) signals. In section 3, we review paleoecological and archaeological syntheses that provide ground truth evidence on early anthropogenic releases of greenhouse gases. The available data document large early anthropogenic emissions consistent with the anthropogenic ice core anomalies, but more information is needed to constrain their size. A final section compares natural and anthropogenic interpretations of the δ 13 C trend in ice core CO 2 . Holocene ice core and ocean sediment trends are anomalous compared to previous interglaciations Paleoecology and archaeology show that early farmers emitted large amounts of CO 2 and CH 4 Large early agricultural emissions are consistent with geochemical constraints |
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For more than a decade, scientists have argued about the warmth of the current interglaciation. Was the warmth of the preindustrial late Holocene natural in origin, the result of orbital changes that had not yet driven the system into a new glacial state? Or was it in considerable degree the result of humans intervening in the climate system through greenhouse gas emissions from early agriculture? Here we summarize new evidence that moves this debate forward by testing both hypotheses. By comparing late Holocene responses to those that occurred during previous interglaciations (in section 2), we assess whether the late Holocene responses look different (and thus anthropogenic) or similar (and thus natural). This comparison reveals anomalous (anthropogenic) signals. In section 3, we review paleoecological and archaeological syntheses that provide ground truth evidence on early anthropogenic releases of greenhouse gases. The available data document large early anthropogenic emissions consistent with the anthropogenic ice core anomalies, but more information is needed to constrain their size. A final section compares natural and anthropogenic interpretations of the δ 13 C trend in ice core CO 2 . Holocene ice core and ocean sediment trends are anomalous compared to previous interglaciations Paleoecology and archaeology show that early farmers emitted large amounts of CO 2 and CH 4 Large early agricultural emissions are consistent with geochemical constraints |
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For more than a decade, scientists have argued about the warmth of the current interglaciation. Was the warmth of the preindustrial late Holocene natural in origin, the result of orbital changes that had not yet driven the system into a new glacial state? Or was it in considerable degree the result of humans intervening in the climate system through greenhouse gas emissions from early agriculture? Here we summarize new evidence that moves this debate forward by testing both hypotheses. By comparing late Holocene responses to those that occurred during previous interglaciations (in section 2), we assess whether the late Holocene responses look different (and thus anthropogenic) or similar (and thus natural). This comparison reveals anomalous (anthropogenic) signals. In section 3, we review paleoecological and archaeological syntheses that provide ground truth evidence on early anthropogenic releases of greenhouse gases. The available data document large early anthropogenic emissions consistent with the anthropogenic ice core anomalies, but more information is needed to constrain their size. A final section compares natural and anthropogenic interpretations of the δ 13 C trend in ice core CO 2 . Holocene ice core and ocean sediment trends are anomalous compared to previous interglaciations Paleoecology and archaeology show that early farmers emitted large amounts of CO 2 and CH 4 Large early agricultural emissions are consistent with geochemical constraints |
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Late Holocene climate: Natural or anthropogenic? |
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Fuller, D. Q Kutzbach, J. E Tzedakis, P. C Kaplan, J. O Ellis, E. C Vavrus, S. J Roberts, C. N Fyfe, R He, F Lemmen, C Woodbridge, J |
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