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      New Ophthalmosaurid Ichthyosaurs from the European Lower Cretaceous Demonstrate Extensive Ichthyosaur Survival across the Jurassic–Cretaceous Boundary

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          Abstract

          Background

          Ichthyosauria is a diverse clade of marine amniotes that spanned most of the Mesozoic. Until recently, most authors interpreted the fossil record as showing that three major extinction events affected this group during its history: one during the latest Triassic, one at the Jurassic–Cretaceous boundary (JCB), and one (resulting in total extinction) at the Cenomanian-Turonian boundary. The JCB was believed to eradicate most of the peculiar morphotypes found in the Late Jurassic, in favor of apparently less specialized forms in the Cretaceous. However, the record of ichthyosaurs from the Berriasian–Barremian interval is extremely limited, and the effects of the end-Jurassic extinction event on ichthyosaurs remains poorly understood.

          Methodology/Principal Findings

          Based on new material from the Hauterivian of England and Germany and on abundant material from the Cambridge Greensand Formation, we name a new ophthalmosaurid, Acamptonectes densus gen. et sp. nov. This taxon shares numerous features with Ophthalmosaurus, a genus now restricted to the Callovian–Berriasian interval. Our phylogenetic analysis indicates that Ophthalmosauridae diverged early in its history into two markedly distinct clades, Ophthalmosaurinae and Platypterygiinae, both of which cross the JCB and persist to the late Albian at least. To evaluate the effect of the JCB extinction event on ichthyosaurs, we calculated cladogenesis, extinction, and survival rates for each stage of the Oxfordian–Barremian interval, under different scenarios. The extinction rate during the JCB never surpasses the background extinction rate for the Oxfordian–Barremian interval and the JCB records one of the highest survival rates of the interval.

          Conclusions/Significance

          There is currently no evidence that ichthyosaurs were affected by the JCB extinction event, in contrast to many other marine groups. Ophthalmosaurid ichthyosaurs remained diverse from their rapid radiation in the Middle Jurassic to their total extinction at the beginning of the Late Cretaceous.

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          Most cited references78

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          Geologic constraints on the macroevolutionary history of marine animals.

          The causes of mass extinctions and the nature of taxonomic radiations are central questions in paleobiology. Several episodes of taxonomic turnover in the fossil record, particularly the major mass extinctions, are generally thought to transcend known biases in the geologic record and are widely interpreted as distinct macroevolutionary phenomena that require unique forcing mechanisms. Here, by using a previously undescribed compilation of the durations of sedimentary rock sequences, I compare the rates of expansion and truncation of preserved marine sedimentary basins to rates of origination and extinction among Phanerozoic marine animal genera. Many features of the highly variable record of taxonomic first and last occurrences in the marine animal fossil record, including the major mass extinctions, the frequency distribution of genus longevities, and short- and long-term patterns of genus diversity, can be predicted on the basis of the temporal continuity and quantity of preserved sedimentary rock. Although these results suggest that geologically mediated sampling biases have distorted macroevolutionary patterns in the fossil record, preservation biases alone cannot easily explain the extent to which the sedimentary record duplicates paleobiological patterns. Instead, these results suggest that the processes responsible for producing variability in the sedimentary rock record, such as plate tectonics and sea-level change, may have been dominant and consistent macroevolutionary forces throughout the Phanerozoic.
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            EVOLUTION OF FISH-SHAPED REPTILES (REPTILIA: ICHTHYOPTERYGIA) IN THEIR PHYSICAL ENVIRONMENTS AND CONSTRAINTS

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              Resetting the evolution of marine reptiles at the Triassic-Jurassic boundary.

              Ichthyosaurs were important marine predators in the Early Jurassic, and an abundant and diverse component of Mesozoic marine ecosystems. Despite their ecological importance, however, the Early Jurassic species represent a reduced remnant of their former significance in the Triassic. Ichthyosaurs passed through an evolutionary bottleneck at, or close to, the Triassic-Jurassic boundary, which reduced their diversity to as few as three or four lineages. Diversity bounced back to some extent in the aftermath of the end-Triassic mass extinction, but disparity remained at less than one-tenth of pre-extinction levels, and never recovered. The group remained at low diversity and disparity for its final 100 Myr. The end-Triassic mass extinction had a previously unsuspected profound effect in resetting the evolution of apex marine predators of the Mesozoic.
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                Author and article information

                Contributors
                Role: Editor
                Journal
                PLoS One
                plos
                plosone
                PLoS ONE
                Public Library of Science (San Francisco, USA )
                1932-6203
                2012
                3 January 2012
                : 7
                : 1
                : e29234
                Affiliations
                [1 ]Geology department, University of Liège, Liège, Belgium
                [2 ]Paleontology Department, Royal Belgian Institute of Natural Sciences, Brussels, Belgium
                [3 ]School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth, United Kingdom
                [4 ]School of Ocean and Earth Sciences, University of Southampton, Southampton, United Kingdom
                [5 ]Staatliches Naturhistorisches Museum, Braunschweig, Germany
                [6 ]Division of Environmental and Evolutionary Biology, School of Life Sciences, College of Medical Veterinary and Life Sciences, University of Glasgow, Glasgow, Scotland
                [7 ]Institut für Geowissenschaften, Ruprecht-Karls-Universität Heidelberg, Heidelberg, Germany
                University of Western Ontario, Canada
                Author notes

                Conceived and designed the experiments: VF. Performed the experiments: VF. Analyzed the data: VF. Contributed reagents/materials/analysis tools: UJ RK FJK. Wrote the paper: VF DN JL RK. Described the Cremlingen specimen: VF MWM JPP. Described the Speeton specimen: VF RMA JT. Described the CAMSM and BMNH specimens: VF.

                [¤a]

                Current address: Tübingen, Germany

                [¤b]

                Current address: National Museums Scotland, Edinburgh, Scotland

                [†]

                Deceased: formerly Department of Geology, University College, Cardiff, UK.

                Article
                PONE-D-11-19735
                10.1371/journal.pone.0029234
                3250416
                22235274
                695b0c58-b4b7-4999-843a-5833de7790c7
                Fischer et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
                History
                : 6 October 2011
                : 22 November 2011
                Page count
                Pages: 23
                Categories
                Research Article
                Biology
                Anatomy and Physiology
                Comparative Anatomy
                Ecology
                Biodiversity
                Species Extinction
                Evolutionary Biology
                Evolutionary Systematics
                Taxonomy
                Animal Taxonomy
                Cladistics
                Phylogenetics
                Earth Sciences
                Paleontology
                Biostratigraphy
                Vertebrate Paleontology

                Uncategorized
                Uncategorized

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