TY - JOUR
T1 - The geological record of ocean acidification
AU - Hönisch, Bärbel
AU - Ridgwell, Andy
AU - Schmidt, Daniela N.
AU - Thomas, Ellen
AU - Gibbs, Samantha J.
AU - Sluijs, Appy
AU - Zeebe, Richard
AU - Kump, Lee
AU - Martindale, Rowan C.
AU - Greene, Sarah E.
AU - Kiessling, Wolfgang
AU - Ries, Justin
AU - Zachos, James C.
AU - Royer, Dana L.
AU - Barker, Stephen
AU - Marchitto, Thomas M.
AU - Moyer, Ryan
AU - Pelejero, Carles
AU - Ziveri, Patrizia
AU - Foster, Gavin L.
AU - Williams, Branwen
PY - 2012/3/2
Y1 - 2012/3/2
N2 - 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 CO 2 release currently taking place.
AB - 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 CO 2 release currently taking place.
U2 - 10.1126/science.1208277
DO - 10.1126/science.1208277
M3 - Review article
SN - 0036-8075
VL - 335
SP - 1058
EP - 1063
JO - Science
JF - Science
IS - 6072
ER -