The Geological Record of Ocean Acidification: Supporting Online Material

Ocean acidification may have severe consequences for marine ecosystems; however, assessing its future impact is difficult because laboratory experiments and field observations are limited by their reduced ecologic complexity and sample period, respectively. In contrast, the geological record contain...

Full description

Bibliographic Details
Main Authors: Hoenisch, Baerbel, Ridgwell, Andy, Schmidt, Daniela N., Thomas, Ellen, Gibbs, Samantha J., Sluijs, Appy, Zeebe, Richard, Martindale, Rowan C., Kump, Lee, Greene, Sarah E., Kiessling, Wolfgang, Ries, Justin, Zachos, James C., Royer, Dana L., Barker, Stephen, Marchitto, Thomas M., Moyer, Ryan, Pelejero, Carles, Ziveri, Patrizia, Foster, Gavin L., Williams, Branwen
Format: Other/Unknown Material
Language:English
Published: 2012
Subjects:
Online Access:https://doi.org/10.7916/D8RX9BD3
id ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/D8RX9BD3
record_format openpolar
spelling ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/D8RX9BD3 2023-05-15T17:48:54+02:00 The Geological Record of Ocean Acidification: Supporting Online Material Hoenisch, Baerbel Ridgwell, Andy Schmidt, Daniela N. Thomas, Ellen Gibbs, Samantha J. Sluijs, Appy Zeebe, Richard Martindale, Rowan C. Kump, Lee Greene, Sarah E. Kiessling, Wolfgang Ries, Justin Zachos, James C. Royer, Dana L. Barker, Stephen Marchitto, Thomas M. Moyer, Ryan Pelejero, Carles Ziveri, Patrizia Foster, Gavin L. Williams, Branwen 2012 https://doi.org/10.7916/D8RX9BD3 English eng https://doi.org/10.7916/D8RX9BD3 Ocean acidification Paleoclimatology Oceanography Climatic changes Global warming Data (information) 2012 ftcolumbiauniv https://doi.org/10.7916/D8RX9BD3 2019-04-04T08:07:31Z Ocean acidification may have severe consequences for marine ecosystems; however, assessing its future impact is difficult because laboratory experiments and field observations are limited by their reduced ecologic complexity and sample period, respectively. In contrast, the geological record contains long-term evidence for a variety of global environmental perturbations, including ocean acidification plus their associated biotic responses. We review events exhibiting evidence for elevated atmospheric CO2, global warming, and ocean acidification over the past ~300 million years of Earth's history, some with contemporaneous extinction or evolutionary turnover among marine calcifiers. Although similarities exist, no past event perfectly parallels future projections in terms of disrupting the balance of ocean carbonate chemistry—a consequence of the unprecedented rapidity of CO2 release currently taking place. Other/Unknown Material Ocean acidification Columbia University: Academic Commons
institution Open Polar
collection Columbia University: Academic Commons
op_collection_id ftcolumbiauniv
language English
topic Ocean acidification
Paleoclimatology
Oceanography
Climatic changes
Global warming
spellingShingle Ocean acidification
Paleoclimatology
Oceanography
Climatic changes
Global warming
Hoenisch, Baerbel
Ridgwell, Andy
Schmidt, Daniela N.
Thomas, Ellen
Gibbs, Samantha J.
Sluijs, Appy
Zeebe, Richard
Martindale, Rowan C.
Kump, Lee
Greene, Sarah E.
Kiessling, Wolfgang
Ries, Justin
Zachos, James C.
Royer, Dana L.
Barker, Stephen
Marchitto, Thomas M.
Moyer, Ryan
Pelejero, Carles
Ziveri, Patrizia
Foster, Gavin L.
Williams, Branwen
The Geological Record of Ocean Acidification: Supporting Online Material
topic_facet Ocean acidification
Paleoclimatology
Oceanography
Climatic changes
Global warming
description Ocean acidification may have severe consequences for marine ecosystems; however, assessing its future impact is difficult because laboratory experiments and field observations are limited by their reduced ecologic complexity and sample period, respectively. In contrast, the geological record contains long-term evidence for a variety of global environmental perturbations, including ocean acidification plus their associated biotic responses. We review events exhibiting evidence for elevated atmospheric CO2, global warming, and ocean acidification over the past ~300 million years of Earth's history, some with contemporaneous extinction or evolutionary turnover among marine calcifiers. Although similarities exist, no past event perfectly parallels future projections in terms of disrupting the balance of ocean carbonate chemistry—a consequence of the unprecedented rapidity of CO2 release currently taking place.
format Other/Unknown Material
author Hoenisch, Baerbel
Ridgwell, Andy
Schmidt, Daniela N.
Thomas, Ellen
Gibbs, Samantha J.
Sluijs, Appy
Zeebe, Richard
Martindale, Rowan C.
Kump, Lee
Greene, Sarah E.
Kiessling, Wolfgang
Ries, Justin
Zachos, James C.
Royer, Dana L.
Barker, Stephen
Marchitto, Thomas M.
Moyer, Ryan
Pelejero, Carles
Ziveri, Patrizia
Foster, Gavin L.
Williams, Branwen
author_facet Hoenisch, Baerbel
Ridgwell, Andy
Schmidt, Daniela N.
Thomas, Ellen
Gibbs, Samantha J.
Sluijs, Appy
Zeebe, Richard
Martindale, Rowan C.
Kump, Lee
Greene, Sarah E.
Kiessling, Wolfgang
Ries, Justin
Zachos, James C.
Royer, Dana L.
Barker, Stephen
Marchitto, Thomas M.
Moyer, Ryan
Pelejero, Carles
Ziveri, Patrizia
Foster, Gavin L.
Williams, Branwen
author_sort Hoenisch, Baerbel
title The Geological Record of Ocean Acidification: Supporting Online Material
title_short The Geological Record of Ocean Acidification: Supporting Online Material
title_full The Geological Record of Ocean Acidification: Supporting Online Material
title_fullStr The Geological Record of Ocean Acidification: Supporting Online Material
title_full_unstemmed The Geological Record of Ocean Acidification: Supporting Online Material
title_sort geological record of ocean acidification: supporting online material
publishDate 2012
url https://doi.org/10.7916/D8RX9BD3
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://doi.org/10.7916/D8RX9BD3
op_doi https://doi.org/10.7916/D8RX9BD3
_version_ 1766155072105873408