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      A new caimanine alligatorid from the Middle Eocene of Southwest Texas and implications for spatial and temporal shifts in Paleogene crocodyliform diversity

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          Abstract

          Dramatic early Cenozoic climatic shifts resulted in faunal reorganization on a global scale. Among vertebrates, multiple groups of mammals (e.g., adapiform and omomyiform primates, mesonychids, taeniodonts, dichobunid artiodactyls) are well known from the Western Interior of North America in the warm, greenhouse conditions of the early Eocene, but a dramatic drop in the diversity of these groups, along with the introduction of more dry-tolerant taxa, occurred near the Eocene–Oligocene boundary. Crocodyliforms underwent a striking loss of diversity at this time as well. Pre-Uintan crocodyliform assemblages in the central Western Interior are characterized by multiple taxa, whereas Chadronian assemblages are depauperate with only Alligator prenasalis previously known. Crocodyliform diversity through the intervening Uintan and Duchesnean is not well understood. The middle Eocene Devil’s Graveyard Formation (DGF) of southwest Texas provides new data from southern latitudes during that crucial period. A new specimen from the middle member of the DGF (late Uintan–Duchesnean) is the most complete cranial material of an alligatorid known from Paleogene deposits outside the Western Interior. We identify this specimen as a caimanine based on notched descending laminae of the pterygoids posterior to the choanae and long descending processes of the exoccipitals that are in contact with the basioccipital tubera. Unlike Eocaiman cavernensis, the anterior palatine process is rounded rather than quadrangular. The relationships and age of this new taxon support the hypothesis that the modern distribution of caimanines represents a contraction of a more expansive early Cenozoic distribution. We hypothesize that the range of caimanines tracked shifting warm, humid climatic conditions that contracted latitudinally toward the hothouse-icehouse transition later in the Eocene.

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          Trends, rhythms, and aberrations in global climate 65 Ma to present.

          Since 65 million years ago (Ma), Earth's climate has undergone a significant and complex evolution, the finer details of which are now coming to light through investigations of deep-sea sediment cores. This evolution includes gradual trends of warming and cooling driven by tectonic processes on time scales of 10(5) to 10(7) years, rhythmic or periodic cycles driven by orbital processes with 10(4)- to 10(6)-year cyclicity, and rare rapid aberrant shifts and extreme climate transients with durations of 10(3) to 10(5) years. Here, recent progress in defining the evolution of global climate over the Cenozoic Era is reviewed. We focus primarily on the periodic and anomalous components of variability over the early portion of this era, as constrained by the latest generation of deep-sea isotope records. We also consider how this improved perspective has led to the recognition of previously unforeseen mechanisms for altering climate.
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            An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics.

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              Middle Miocene Southern Ocean cooling and Antarctic cryosphere expansion.

              Magnesium/calcium data from Southern Ocean planktonic foraminifera demonstrate that high-latitude (approximately 55 degrees S) southwest Pacific sea surface temperatures (SSTs) cooled 6 degrees to 7 degrees C during the middle Miocene climate transition (14.2 to 13.8 million years ago). Stepwise surface cooling is paced by eccentricity forcing and precedes Antarctic cryosphere expansion by approximately 60 thousand years, suggesting the involvement of additional feedbacks during this interval of inferred low-atmospheric partial pressure of CO2 (pCO2). Comparing SSTs and global carbon cycling proxies challenges the notion that episodic pCO2 drawdown drove this major Cenozoic climate transition. SST, salinity, and ice-volume trends suggest instead that orbitally paced ocean circulation changes altered meridional heat/vapor transport, triggering ice growth and global cooling.
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                Author and article information

                Contributors
                Journal
                PeerJ
                PeerJ
                PeerJ
                PeerJ
                PeerJ
                PeerJ Inc. (San Diego, USA )
                2167-8359
                15 January 2021
                2021
                : 9
                : e10665
                Affiliations
                [1 ]Department of Geosciences, Virginia Polytechnic Institute and State University (Virginia Tech) , Blacksburg, VA, USA
                [2 ]Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin , Austin, TX, USA
                [3 ]Department of Earth and Environmental Sciences, University of Iowa , Iowa City, IA, USA
                [4 ]Department of Anthropology, The University of Texas at Austin , Austin, TX, USA
                [5 ]Jackson School Museum of Earth History, The University of Texas at Austin , Austin, TX, USA
                Author information
                http://orcid.org/0000-0002-6473-8691
                Article
                10665
                10.7717/peerj.10665
                7812925
                33520458
                3623ed8e-3b2b-4a92-8c19-18cb4a31d77b
                © 2021 Stocker et al.

                This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, reproduction and adaptation in any medium and for any purpose provided that it is properly attributed. For attribution, the original author(s), title, publication source (PeerJ) and either DOI or URL of the article must be cited.

                History
                : 15 July 2020
                : 8 December 2020
                Funding
                Funded by: The Jackson School of Geosciences, The University of Texas at Austin
                Funded by: UT College of Liberal Arts, the Society of Vertebrate Paleontology
                Funded by: Department of Geosciences at Virginia Tech
                The Jackson School of Geosciences, The University of Texas at Austin (William Powers, Jr. Presidential Graduate Fellowship to Michelle R. Stocker), the UT College of Liberal Arts, the Society of Vertebrate Paleontology (Jackson School of Geosciences Student Member Travel Grant to Michelle R. Stocker), and the Department of Geosciences at Virginia Tech provided funding for this research. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
                Categories
                Biodiversity
                Paleontology
                Taxonomy
                Zoology

                cenozoic,caimaninae,diversity,climate change,fossils,devil’s graveyard formation,species distribution

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