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Items: 1 to 20 of 106

1.

Oceanographic controls on the diversity and extinction of planktonic foraminifera.

Peters SE, Kelly DC, Fraass AJ.

Nature. 2013 Jan 17;493(7432):398-401. doi: 10.1038/nature11815.

PMID:
23302802
2.

Evolution: A history of give and take.

Holland SM.

Nature. 2013 Jan 17;493(7432):308-9. doi: 10.1038/nature11851. No abstract available.

PMID:
23302799
3.

Planktonic foraminifera as bio-indicators for monitoring the climatic changes that have occurred over the past 2000 years in the southeastern Tyrrhenian Sea.

Lirer F, Sprovieri M, Vallefuoco M, Ferraro L, Pelosi N, Giordano L, Capotondi L.

Integr Zool. 2014 Aug;9(4):542-54. doi: 10.1111/1749-4877.12083.

PMID:
24382193
4.

Interplay between changing climate and species' ecology drives macroevolutionary dynamics.

Ezard TH, Aze T, Pearson PN, Purvis A.

Science. 2011 Apr 15;332(6027):349-51. doi: 10.1126/science.1203060.

5.

The impact of Cenozoic cooling on assemblage diversity in planktonic foraminifera.

Fenton IS, Pearson PN, Dunkley Jones T, Farnsworth A, Lunt DJ, Markwick P, Purvis A.

Philos Trans R Soc Lond B Biol Sci. 2016 Apr 5;371(1691):20150224. doi: 10.1098/rstb.2015.0224.

6.

Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.

Anagnostou E, John EH, Edgar KM, Foster GL, Ridgwell A, Inglis GN, Pancost RD, Lunt DJ, Pearson PN.

Nature. 2016 May 19;533(7603):380-4. doi: 10.1038/nature17423.

7.

Cryptic species of planktonic foraminifera: their effect on palaeoceanographic reconstructions.

Kucera M, Darling KF.

Philos Trans A Math Phys Eng Sci. 2002 Apr 15;360(1793):695-718.

8.

Phanerozoic Earth system evolution and marine biodiversity.

Hannisdal B, Peters SE.

Science. 2011 Nov 25;334(6059):1121-4. doi: 10.1126/science.1210695.

9.

Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.

Gibbs SJ, Bown PR, Sessa JA, Bralower TJ, Wilson PA.

Science. 2006 Dec 15;314(5806):1770-3.

10.

Epicontinental seas versus open-ocean settings: the kinetics of mass extinction and origination.

Miller AI, Foote M.

Science. 2009 Nov 20;326(5956):1106-9. doi: 10.1126/science.1180061.

11.

Eocene global warming events driven by ventilation of oceanic dissolved organic carbon.

Sexton PF, Norris RD, Wilson PA, Pälike H, Westerhold T, Röhl U, Bolton CT, Gibbs S.

Nature. 2011 Mar 17;471(7338):349-52. doi: 10.1038/nature09826.

PMID:
21412336
12.

Greenhouse-icehouse transition in the Late Ordovician marks a step change in extinction regime in the marine plankton.

Crampton JS, Cooper RA, Sadler PM, Foote M.

Proc Natl Acad Sci U S A. 2016 Feb 9;113(6):1498-503. doi: 10.1073/pnas.1519092113.

13.

End-Cretaceous marine mass extinction not caused by productivity collapse.

Alegret L, Thomas E, Lohmann KC.

Proc Natl Acad Sci U S A. 2012 Jan 17;109(3):728-32. doi: 10.1073/pnas.1110601109.

14.

A phylogeny of Cenozoic macroperforate planktonic foraminifera from fossil data.

Aze T, Ezard TH, Purvis A, Coxall HK, Stewart DR, Wade BS, Pearson PN.

Biol Rev Camb Philos Soc. 2011 Nov;86(4):900-27. doi: 10.1111/j.1469-185X.2011.00178.x.

PMID:
21492379
15.
16.

Oceanographic dynamics and the end of the last interglacial in the subpolar North Atlantic.

Mokeddem Z, McManus JF, Oppo DW.

Proc Natl Acad Sci U S A. 2014 Aug 5;111(31):11263-8. doi: 10.1073/pnas.1322103111.

17.

Ocean currents generate large footprints in marine palaeoclimate proxies.

van Sebille E, Scussolini P, Durgadoo JV, Peeters FJ, Biastoch A, Weijer W, Turney C, Paris CB, Zahn R.

Nat Commun. 2015 Mar 4;6:6521. doi: 10.1038/ncomms7521. Review.

PMID:
25735516
18.

Upper-ocean-to-atmosphere radiocarbon offsets imply fast deglacial carbon dioxide release.

Rose KA, Sikes EL, Guilderson TP, Shane P, Hill TM, Zahn R, Spero HJ.

Nature. 2010 Aug 26;466(7310):1093-7. doi: 10.1038/nature09288.

PMID:
20740012
19.

Surviving rapid climate change in the deep sea during the Paleogene hyperthermals.

Foster LC, Schmidt DN, Thomas E, Arndt S, Ridgwell A.

Proc Natl Acad Sci U S A. 2013 Jun 4;110(23):9273-6. doi: 10.1073/pnas.1300579110.

20.

Climate change. Atlantic current can shut down for centuries, disrupting climate.

Kerr RA.

Science. 2014 Feb 21;343(6173):831. doi: 10.1126/science.343.6173.831. No abstract available.

PMID:
24558140

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