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  • 1
    Publication Date: 2013-08-03
    Description: The future impacts of anthropogenic global change on marine ecosystems are highly uncertain, but insights can be gained from past intervals of high atmospheric carbon dioxide partial pressure. The long-term geological record reveals an early Cenozoic warm climate that supported smaller polar ecosystems, few coral-algal reefs, expanded shallow-water platforms, longer food chains with less energy for top predators, and a less oxygenated ocean than today. The closest analogs for our likely future are climate transients, 10,000 to 200,000 years in duration, that occurred during the long early Cenozoic interval of elevated warmth. Although the future ocean will begin to resemble the past greenhouse world, it will retain elements of the present "icehouse" world long into the future. Changing temperatures and ocean acidification, together with rising sea level and shifts in ocean productivity, will keep marine ecosystems in a state of continuous change for 100,000 years.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Norris, R D -- Turner, S Kirtland -- Hull, P M -- Ridgwell, A -- New York, N.Y. -- Science. 2013 Aug 2;341(6145):492-8. doi: 10.1126/science.1240543.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA. rnorris@ucsd.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23908226" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Biological Evolution ; *Climate Change/history ; *Ecosystem ; Greenhouse Effect ; History, Ancient ; *Oceans and Seas ; *Seawater ; Temperature ; Tidal Waves ; Vertebrates
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2012-08-31
    Description: Atmospheric carbon dioxide concentrations and climate are regulated on geological timescales by the balance between carbon input from volcanic and metamorphic outgassing and its removal by weathering feedbacks; these feedbacks involve the erosion of silicate rocks and organic-carbon-bearing rocks. The integrated effect of these processes is reflected in the calcium carbonate compensation depth, which is the oceanic depth at which calcium carbonate is dissolved. Here we present a carbonate accumulation record that covers the past 53 million years from a depth transect in the equatorial Pacific Ocean. The carbonate compensation depth tracks long-term ocean cooling, deepening from 3.0-3.5 kilometres during the early Cenozoic (approximately 55 million years ago) to 4.6 kilometres at present, consistent with an overall Cenozoic increase in weathering. We find large superimposed fluctuations in carbonate compensation depth during the middle and late Eocene. Using Earth system models, we identify changes in weathering and the mode of organic-carbon delivery as two key processes to explain these large-scale Eocene fluctuations of the carbonate compensation depth.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Palike, Heiko -- Lyle, Mitchell W -- Nishi, Hiroshi -- Raffi, Isabella -- Ridgwell, Andy -- Gamage, Kusali -- Klaus, Adam -- Acton, Gary -- Anderson, Louise -- Backman, Jan -- Baldauf, Jack -- Beltran, Catherine -- Bohaty, Steven M -- Bown, Paul -- Busch, William -- Channell, Jim E T -- Chun, Cecily O J -- Delaney, Margaret -- Dewangan, Pawan -- Dunkley Jones, Tom -- Edgar, Kirsty M -- Evans, Helen -- Fitch, Peter -- Foster, Gavin L -- Gussone, Nikolaus -- Hasegawa, Hitoshi -- Hathorne, Ed C -- Hayashi, Hiroki -- Herrle, Jens O -- Holbourn, Ann -- Hovan, Steve -- Hyeong, Kiseong -- Iijima, Koichi -- Ito, Takashi -- Kamikuri, Shin-ichi -- Kimoto, Katsunori -- Kuroda, Junichiro -- Leon-Rodriguez, Lizette -- Malinverno, Alberto -- Moore, Ted C Jr -- Murphy, Brandon H -- Murphy, Daniel P -- Nakamura, Hideto -- Ogane, Kaoru -- Ohneiser, Christian -- Richter, Carl -- Robinson, Rebecca -- Rohling, Eelco J -- Romero, Oscar -- Sawada, Ken -- Scher, Howie -- Schneider, Leah -- Sluijs, Appy -- Takata, Hiroyuki -- Tian, Jun -- Tsujimoto, Akira -- Wade, Bridget S -- Westerhold, Thomas -- Wilkens, Roy -- Williams, Trevor -- Wilson, Paul A -- Yamamoto, Yuhji -- Yamamoto, Shinya -- Yamazaki, Toshitsugu -- Zeebe, Richard E -- England -- Nature. 2012 Aug 30;488(7413):609-14. doi: 10.1038/nature11360.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK. hpaelike@marum.de〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/22932385" target="_blank"〉PubMed〈/a〉
    Keywords: *Altitude ; Atmosphere/chemistry ; Calcium Carbonate/*analysis ; *Carbon Cycle ; Carbon Dioxide/analysis ; Diatoms/metabolism ; Foraminifera/metabolism ; Geologic Sediments/chemistry ; Global Warming/history/statistics & numerical data ; History, 21st Century ; History, Ancient ; Marine Biology ; Oxygen/metabolism ; Pacific Ocean ; Seawater/*chemistry ; Temperature
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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