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dc.contributor.authorMonteiro, F. M.
dc.contributor.authorBach, L. T.
dc.contributor.authorBrownlee, C.
dc.contributor.authorBown, P.
dc.contributor.authorRickaby, R. E. M.
dc.contributor.authorPoulton, A. J.
dc.contributor.authorTyrrell, T.
dc.contributor.authorBeaufort, L.
dc.contributor.authorGibbs, S.
dc.contributor.authorGutowska, M. A.
dc.contributor.authorLee, R.
dc.contributor.authorRiebesell, U.
dc.contributor.authorYoung, J.
dc.contributor.authorRidgwell, A.
dc.contributor.authorDutkiewicz, Stephanie
dc.date.accessioned2018-02-13T17:39:00Z
dc.date.available2018-02-13T17:39:00Z
dc.date.issued2016-07
dc.date.submitted2015-12
dc.identifier.issn2375-2548
dc.identifier.urihttp://hdl.handle.net/1721.1/113623
dc.description.abstractCalcifying marine phytoplankton—coccolithophores— are some of the most successful yet enigmatic organisms in the ocean and are at risk from global change. To better understand how they will be affected, we need to know “why” coccolithophores calcify. We review coccolithophorid evolutionary history and cell biology as well as insights from recent experiments to provide a critical assessment of the costs and benefits of calcification. We conclude that calcification has high energy demands and that coccolithophores might have calcified initially to reduce grazing pressure but that additional benefits such as protection from photodamage and viral/bacterial attack further explain their high diversity and broad spectrum ecology. The cost-benefit aspect of these traits is illustrated by novel ecosystem modeling, although conclusive observations remain limited. In the future ocean, the trade-off between changing ecological and physiological costs of calcification and their benefits will ultimately decide how this important group is affected by ocean acidification and global warming.en_US
dc.description.sponsorshipNational Science Foundation (U.S.) (NSF [OCE-1434007)en_US
dc.publisherAmerican Association for the Advancement of Science (AAAS)en_US
dc.relation.isversionofhttp://dx.doi.org/10.1126/sciadv.1501822en_US
dc.rightsCreative Commons Attribution 4.0 International Licenseen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.titleWhy marine phytoplankton calcifyen_US
dc.typeArticleen_US
dc.identifier.citationMonteiro, F. M., L. T. Bach, C. Brownlee, P. Bown, R. E. M. Rickaby, A. J. Poulton, T. Tyrrell, et al. “Why Marine Phytoplankton Calcify.” Science Advances 2, no. 7 (July 13, 2016): e1501822–e1501822.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Center for Global Change Scienceen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.mitauthorDutkiewicz, Stephanie
dc.relation.journalScience Advancesen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2018-02-09T18:52:26Z
dspace.orderedauthorsMonteiro, F. M.; Bach, L. T.; Brownlee, C.; Bown, P.; Rickaby, R. E. M.; Poulton, A. J.; Tyrrell, T.; Beaufort, L.; Dutkiewicz, S.; Gibbs, S.; Gutowska, M. A.; Lee, R.; Riebesell, U.; Young, J.; Ridgwell, A.en_US
dspace.embargo.termsNen_US
mit.licensePUBLISHER_POLICYen_US


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