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Items: 1 to 20 of 124

1.

Climate change and the selective signature of the Late Ordovician mass extinction.

Finnegan S, Heim NA, Peters SE, Fischer WW.

Proc Natl Acad Sci U S A. 2012 May 1;109(18):6829-34. doi: 10.1073/pnas.1117039109. Epub 2012 Apr 17.

2.

Rapid recovery from the Late Ordovician mass extinction.

Krug AZ, Patzkowsky ME.

Proc Natl Acad Sci U S A. 2004 Dec 21;101(51):17605-10. Epub 2004 Dec 13.

3.

Biogeographic and bathymetric determinants of brachiopod extinction and survival during the Late Ordovician mass extinction.

Finnegan S, Rasmussen CM, Harper DA.

Proc Biol Sci. 2016 Apr 27;283(1829). pii: 20160007. doi: 10.1098/rspb.2016.0007.

PMID:
27122567
4.

The magnitude and duration of Late Ordovician-Early Silurian glaciation.

Finnegan S, Bergmann K, Eiler JM, Jones DS, Fike DA, Eisenman I, Hughes NC, Tripati AK, Fischer WW.

Science. 2011 Feb 18;331(6019):903-6. doi: 10.1126/science.1200803. Epub 2011 Jan 27.

5.

Out of the tropics, but how? Fossils, bridge species, and thermal ranges in the dynamics of the marine latitudinal diversity gradient.

Jablonski D, Belanger CL, Berke SK, Huang S, Krug AZ, Roy K, Tomasovych A, Valentine JW.

Proc Natl Acad Sci U S A. 2013 Jun 25;110(26):10487-94. doi: 10.1073/pnas.1308997110. Epub 2013 Jun 12.

6.

Phanerozoic Earth system evolution and marine biodiversity.

Hannisdal B, Peters SE.

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

7.

Response of beta diversity to pulses of Ordovician-Silurian mass extinction.

Darroch SA, Wagner PJ.

Ecology. 2015 Feb;96(2):532-49.

PMID:
26240874
8.

Biodiversity tracks temperature over time.

Mayhew PJ, Bell MA, Benton TG, McGowan AJ.

Proc Natl Acad Sci U S A. 2012 Sep 18;109(38):15141-5. Epub 2012 Sep 4.

9.

Extinctions. Paleontological baselines for evaluating extinction risk in the modern oceans.

Finnegan S, Anderson SC, Harnik PG, Simpson C, Tittensor DP, Byrnes JE, Finkel ZV, Lindberg DR, Liow LH, Lockwood R, Lotze HK, McClain CR, McGuire JL, O'Dea A, Pandolfi JM.

Science. 2015 May 1;348(6234):567-70. doi: 10.1126/science.aaa6635.

10.

Chapter 4. Susceptibility of sharks, rays and chimaeras to global extinction.

Field IC, Meekan MG, Buckworth RC, Bradshaw CJ.

Adv Mar Biol. 2009;56:275-363. doi: 10.1016/S0065-2881(09)56004-X.

PMID:
19895977
11.

Phylogenetic and biogeographic analysis of sphaerexochine trilobites.

Congreve CR, Lieberman BS.

PLoS One. 2011;6(6):e21304. doi: 10.1371/journal.pone.0021304. Epub 2011 Jun 27.

12.

Fossil preservation and the stratigraphic ranges of taxa.

Foote M, Raup DM.

Paleobiology. 1996 Spring;22(2):121-40.

PMID:
11539203
13.

Determinants of extinction in the fossil record.

Peters SE, Foote M.

Nature. 2002 Mar 28;416(6879):420-4.

PMID:
11919629
14.

Species-specific responses of Late Quaternary megafauna to climate and humans.

Lorenzen ED, Nogués-Bravo D, Orlando L, Weinstock J, Binladen J, Marske KA, Ugan A, Borregaard MK, Gilbert MT, Nielsen R, Ho SY, Goebel T, Graf KE, Byers D, Stenderup JT, Rasmussen M, Campos PF, Leonard JA, Koepfli KP, Froese D, Zazula G, Stafford TW Jr, Aaris-Sørensen K, Batra P, Haywood AM, Singarayer JS, Valdes PJ, Boeskorov G, Burns JA, Davydov SP, Haile J, Jenkins DL, Kosintsev P, Kuznetsova T, Lai X, Martin LD, McDonald HG, Mol D, Meldgaard M, Munch K, Stephan E, Sablin M, Sommer RS, Sipko T, Scott E, Suchard MA, Tikhonov A, Willerslev R, Wayne RK, Cooper A, Hofreiter M, Sher A, Shapiro B, Rahbek C, Willerslev E.

Nature. 2011 Nov 2;479(7373):359-64. doi: 10.1038/nature10574.

15.

Environmental determinants of extinction selectivity in the fossil record.

Peters SE.

Nature. 2008 Jul 31;454(7204):626-9. doi: 10.1038/nature07032. Epub 2008 Jun 15.

PMID:
18552839
16.

The effect of geographic range on extinction risk during background and mass extinction.

Payne JL, Finnegan S.

Proc Natl Acad Sci U S A. 2007 Jun 19;104(25):10506-11. Epub 2007 Jun 11.

17.

Diversity dynamics of Miocene mammals in relation to the history of tectonism and climate.

Finarelli JA, Badgley C.

Proc Biol Sci. 2010 Sep 7;277(1694):2721-6. doi: 10.1098/rspb.2010.0348. Epub 2010 Apr 28.

18.

Geologic drivers of late ordovician faunal change in laurentia: investigating links between tectonics, speciation, and biotic invasions.

Wright DF, Stigall AL.

PLoS One. 2013 Jul 15;8(7):e68353. doi: 10.1371/journal.pone.0068353. Print 2013.

19.

Did cooling oceans trigger Ordovician biodiversification? Evidence from conodont thermometry.

Trotter JA, Williams IS, Barnes CR, Lécuyer C, Nicoll RS.

Science. 2008 Jul 25;321(5888):550-4. doi: 10.1126/science.1155814.

20.

Ordovician faunas of Burgess Shale type.

Van Roy P, Orr PJ, Botting JP, Muir LA, Vinther J, Lefebvre B, el Hariri K, Briggs DE.

Nature. 2010 May 13;465(7295):215-8. doi: 10.1038/nature09038.

PMID:
20463737
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