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dc.contributor.authorYasuhara, Moriaki
dc.contributor.authorHuang, Huai-Hsuan May
dc.contributor.authorHull, Pincelli
dc.contributor.authorRillo, Marina C.
dc.contributor.authorCondamine, Fabien L.
dc.contributor.authorTittensor, Derek P.
dc.contributor.authorKučera, Michal
dc.contributor.authorCostello, Mark
dc.contributor.authorFinnegan, Seth
dc.contributor.authorO’Dea, Aaron
dc.contributor.authorHong, Yuanyuan
dc.contributor.authorBonebrake, Timothy C.
dc.contributor.authorMcKenzie, N. Ryan
dc.contributor.authorDoi, Hideyuki
dc.contributor.authorWei, Chih-Lin
dc.contributor.authorKubota, Yasuhiro
dc.contributor.authorSaupe, Erin E.
dc.date.accessioned2021-03-01T09:52:20Z
dc.date.available2021-03-01T09:52:20Z
dc.date.created2020-11-18T00:21:59Z
dc.date.issued2020
dc.identifier.citationYasuhara, M., Huang, H.-H. M., Hull, P., Rillo, M. C., Condamine, F. L., Tittensor, D. P. ... Saupe, E. E. (2020). Time machine biology: cross-timescale integration of ecology, evolution, and oceanography. Oceanography, 33(2), 16-28. doi:en_US
dc.identifier.issn2377-617X
dc.identifier.urihttps://hdl.handle.net/11250/2730854
dc.description.abstractDirect observations of marine ecosystems are inherently limited in their temporal scope. Yet, ongoing global anthropogenic change urgently requires improved understanding of long-term baselines, greater insight into the relationship between climate and biodiversity, and knowledge of the evolutionary consequences of our actions. Sediment cores can provide this understanding by linking data on the responses of marine biota to reconstructions of past environmental and climatic change. Given continuous sedimentation and robust age control, studies of sediment cores have the potential to constrain the state and dynamics of past climates and ecosystems on time­scales of centuries to millions of years. Here, we review the development and recent advances in “ocean drilling paleobiology”—a synthetic science with potential to illuminate the interplay and relative importance of ecological and evolutionary factors during times of global change. Climate, specifically temperature, appears to control Cenozoic marine ecosystems on million-year, millennial, centennial, and anthropogenic time­scales. Although certainly not the only factor controlling biodiversity dynamics, the effect size of temperature is large for both pelagic and deep-sea ecosystems.en_US
dc.language.isoengen_US
dc.publisherOceanography Societyen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleTime machine biology : cross-timescale integration of ecology, evolution, and oceanographyen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400en_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Geofag: 450en_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Økologi: 488en_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Marinbiologi: 497en_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Oseanografi: 452en_US
dc.source.pagenumber16-28en_US
dc.source.volume33en_US
dc.source.journalOceanographyen_US
dc.source.issue2en_US
dc.identifier.doi10.5670/oceanog.2020.225
dc.identifier.cristin1848984
dc.relation.projectAndre: Research Grants Council of Hong Kongen_US
dc.relation.projectAndre: University of Hong Kongen_US


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