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The Miocene: The Fu...
The Miocene: The Future of the Past
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- Steinthorsdottir, Margret (författare)
- Naturhistoriska riksmuseet,Enheten för paleobiologi,Bolin Centre for Climate Research, Stockholm University
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- Coxall, H. K. (författare)
- Bolin Centre for Climate Research Stockholm University Stockholm Sweden;Department of Geological Sciences Stockholm University Stockholm Sweden
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- de Boer, A. M. (författare)
- Bolin Centre for Climate Research Stockholm University Stockholm Sweden;Department of Geological Sciences Stockholm University Stockholm Sweden
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- Huber, M. (författare)
- Department of Earth Atmospheric and Planetary Sciences Purdue University West Lafayette IN USA
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- Barbolini, N. (författare)
- Bolin Centre for Climate Research Stockholm University Stockholm Sweden;Department of Ecology Environment and Plant Sciences Stockholm University Stockholm Sweden
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- Bradshaw, C. D. (författare)
- The Global Systems Institute University of Exeter Exeter UK;Met Office Hadley Centre Exeter UK
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- Burls, N. J. (författare)
- Department of Atmospheric Oceanic and Earth Sciences and the Center for Ocean‐Land‐Atmosphere Studies George Mason University Fairfax, VA USA
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- Feakins, S. J. (författare)
- Department of Earth Sciences University of Southern California Los Angeles CA USA
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- Gasson, E. (författare)
- School of Geographical Sciences University of Bristol Bristol UK
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- Henderiks, J. (författare)
- Department of Earth Sciences Uppsala University Uppsala Sweden
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- Holbourn, A. E. (författare)
- Institute of Geosciences Christian‐Albrechts‐University Kiel Germany
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- Kiel, S. (författare)
- Naturhistoriska riksmuseet,Enheten för paleobiologi,Department of Palaeobiology Swedish Museum of Natural History Stockholm Sweden;Bolin Centre for Climate Research Stockholm University Stockholm Sweden
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- Kohn, M. J. (författare)
- Department of Geosciences Boise State University Boise ID USA
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- Knorr, G. (författare)
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Bremerhaven Germany
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- Kürschner, W. M. (författare)
- Department of Geoscience University of Oslo Oslo Norway
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- Lear, C. H. (författare)
- School of Earth and Ocean Sciences Cardiff University Cardiff UK
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- Liebrand, D. (författare)
- MARUM – Center for Marine and Environmental Sciences University of Bremen Bremen Germany
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- Lunt, D. J. (författare)
- School of Geographical Sciences University of Bristol Bristol UK
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- Mörs, Thomas, 1962- (författare)
- Naturhistoriska riksmuseet,Enheten för paleobiologi
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- Pearson, P. N. (författare)
- School of Earth and Ocean Sciences Cardiff University Cardiff UK
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- Pound, M. J. (författare)
- Department of Geography and Environmental Sciences Northumbria University Newcastle upon Tyne UK
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- Stoll, H. (författare)
- Earth Science Department ETH Zürich Zürich Switzerland
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- Strömberg, C. A. E. (författare)
- Department of Biology and Burke Museum of Natural History and Culture University of Washington Seattle WA USA
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(creator_code:org_t)
- 2021-04-27
- 2021
- Engelska.
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Ingår i: Paleoceanography and Paleoclimatology. - : American Geophysical Union (AGU). - 2572-4517 .- 2572-4525. ; 36:4
- Relaterad länk:
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https://doi.org/10.1...
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https://nrm.diva-por... (primary) (Raw object)
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https://onlinelibrar...
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https://urn.kb.se/re...
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https://doi.org/10.1...
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Abstract
Ämnesord
Stäng
- The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative to today. Continental configurations and mountain topography transitioned toward modern conditions, and many flora and fauna evolved into the same taxa that exist today. Miocene climate was dynamic: long periods of early and late glaciation bracketed a ∼2 Myr greenhouse interval—the Miocene Climatic Optimum (MCO). Floras, faunas, ice sheets, precipitation, pCO2, and ocean and atmospheric circulation mostly (but not ubiquitously) covaried with these large changes in climate. With higher temperatures and moderately higher pCO2 (∼400–600 ppm), the MCO has been suggested as a particularly appropriate analog for future climate scenarios, and for assessing the predictive accuracy of numerical climate models—the same models that are used to simulate future climate. Yet, Miocene conditions have proved difficult to reconcile with models. This implies either missing positive feedbacks in the models, a lack of knowledge of past climate forcings, or the need for re-interpretation of proxies, which might mitigate the model-data discrepancy. Our understanding of Miocene climatic, biogeochemical, and oceanic changes on broad spatial and temporal scales is still developing. New records documenting the physical, chemical, and biotic aspects of the Earth system are emerging, and together provide a more comprehensive understanding of this important time interval. Here, we review the state-of-the-art in Miocene climate, ocean circulation, biogeochemical cycling, ice sheet dynamics, and biotic adaptation research as inferred through proxy observations and modeling studies.
Ämnesord
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Annan geovetenskap och miljövetenskap (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Other Earth and Related Environmental Sciences (hsv//eng)
Nyckelord
- Paleontology
- Atmospheric Science
- Oceanography
- Miocene
- Climate
- Ecosystems and species history
- Ekosystem och arthistoria
Publikations- och innehållstyp
- ref (ämneskategori)
- art (ämneskategori)
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Till lärosätets databas
- Av författaren/redakt...
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Steinthorsdottir ...
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Coxall, H. K.
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de Boer, A. M.
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Huber, M.
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Barbolini, N.
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Bradshaw, C. D.
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visa fler...
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Burls, N. J.
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Feakins, S. J.
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Gasson, E.
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Henderiks, J.
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Holbourn, A. E.
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Kiel, S.
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Kohn, M. J.
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Knorr, G.
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Kürschner, W. M.
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Lear, C. H.
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Liebrand, D.
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Lunt, D. J.
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Mörs, Thomas, 19 ...
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Pearson, P. N.
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Pound, M. J.
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Stoll, H.
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Strömberg, C. A. ...
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visa färre...
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