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dc.contributor.authorPrice, S. A.
dc.contributor.authorSchmitz, L.
dc.contributor.authorOufiero, C. E.
dc.contributor.authorEytan, Ron I.
dc.contributor.authorDornburg, A.
dc.contributor.authorSmith, William Leo
dc.contributor.authorFriedman, Matt
dc.contributor.authorNear, Thomas J.
dc.contributor.authorWainwright, P. C.
dc.date.accessioned2014-06-04T15:04:59Z
dc.date.available2014-06-04T15:04:59Z
dc.date.issued2014-05-22
dc.identifier.citationPrice, S. A.; L. Schmitz, C. E. Oufiero, R. I. Eytan, A. Dornburg, W. L. Smith, M. Friedman, T. J. Near, P. C. Wainwright. “Two waves of colonization straddling the K–Pg boundary formed the modern reef fish fauna.” Proc Biol Sci. 2014 May 22; 281(1783): 20140321. htttp://dx.doi.org/10.1098/rspb.2014.0321
dc.identifier.urihttp://hdl.handle.net/1808/13859
dc.description.abstractLiving reef fishes are one of the most diverse vertebrate assemblages on Earth. Despite its prominence and ecological importance, the origins and assembly of the reef fish fauna is poorly described. A patchy fossil record suggests that the major colonization of reef habitats must have occurred in the Late Cretaceous and early Palaeogene, with the earliest known modern fossil coral reef fish assemblage dated to 50 Ma. Using a phylogenetic approach, we analysed the early evolutionary dynamics of modern reef fishes. We find that reef lineages successively colonized reef habitats throughout the Late Cretaceous and early Palaeogene. Two waves of invasion were accompanied by increasing morphological convergence: one in the Late Cretaceous from 90 to 72 Ma and the other immediately following the end-Cretaceous mass extinction. The surge in reef invasions after the Cretaceous–Palaeogene boundary continued for 10 Myr, after which the pace of transitions to reef habitats slowed. Combined, these patterns match a classic niche-filling scenario: early transitions to reefs were made rapidly by morphologically distinct lineages and were followed by a decrease in the rate of invasions and eventual saturation of morphospace. Major alterations in reef composition, distribution and abundance, along with shifts in climate and oceanic currents, occurred during the Late Cretaceous and early Palaeogene interval. A causal mechanism between these changes and concurrent episodes of reef invasion remains obscure, but what is clear is that the broad framework of the modern reef fish fauna was in place within 10 Myr of the end-Cretaceous extinction.
dc.description.sponsorshipWork was supported by NSF grant nos. DEB-1061981 and DEB-0717009 to P.C.W., DEB-1061806 and DEB-1110552 to T.J.N. and DEB-1060869 and EF-0732642 to W.L.S., and NERC grant no. NE/I005536/1 to M.F.
dc.publisherRoyal Society Publishing
dc.rights© 2014 The Authors. Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/3.0/, which permits unrestricted use, provided the original author and source are credited.
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/
dc.subjectMacroevolution
dc.subjectreef fishes
dc.subjectCretaceous-Palaeogene mass extinction
dc.subjectniche-filling models
dc.titleTwo waves of colonization straddling the K–Pg boundary formed the modern reef fish fauna
dc.typeArticle
kusw.kuauthorFriedman, M.
kusw.kudepartmentDepartment of Ecology and Evolutionary Biology
kusw.oastatusfullparticipation
dc.identifier.doi10.1098/rspb.2014.0321
kusw.oaversionScholarly/refereed, publisher version
kusw.oapolicyThis item meets KU Open Access policy criteria.
dc.rights.accessrightsopenAccess


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© 2014 The Authors. Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/3.0/, which permits unrestricted use, provided the original author and source are credited.
Except where otherwise noted, this item's license is described as: © 2014 The Authors. Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/3.0/, which permits unrestricted use, provided the original author and source are credited.