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      Tiny vampires in ancient seas: evidence for predation via perforation in fossils from the 780–740 million-year-old Chuar Group, Grand Canyon, USA

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          Abstract

          One explanation for the Early Neoproterozoic expansion of eukaryotes is the appearance of eukaryovorous predators—i.e. protists that preyed on other protists. Evidence for eukaryovory at this time, however, is indirect, based on inferences from character state reconstructions and molecular clocks, and on the presence of possible defensive structures in some protistan fossils. Here I describe 0.1–3.4 µm circular holes in seven species of organic-walled microfossils from the 780–740 million-year-old Chuar Group, Grand Canyon, Arizona, USA, that are similar to those formed today by predatory protists that perforate the walls of their prey to consume the contents inside. Although best known in the vampyrellid amoebae, this ‘vampire-like’ behaviour is widespread among eukaryotes, making it difficult to infer confidently the identity of the predator. Nonetheless, the identity of the prey is clear: some—and perhaps all—of the fossils are eukaryotes. These holes thus provide the oldest direct evidence for predation on eukaryotes. Larger circular and half-moon-shaped holes in vase-shaped microfossils from the upper part of the unit may also be the work of ‘tiny vampires’, suggesting a diversity of eukaryovorous predators lived in the ancient Chuar sea.

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          The Mesozoic marine revolution: evidence from snails, predators and grazers

          Tertiary and Recent marine gastropods include in their ranks a complement of mechanically sturdy forms unknown in earlier epochs. Open coiling, planispiral coiling, and umbilici detract from shell sturdiness, and were commoner among Paleozoic and Early Mesozoic gastropods than among younger forms. Strong external sculpture, narrow elongate apertures, and apertural dentition promote resistance to crushing predation and are primarily associated with post-Jurassic mesogastropods, neogastropods, and neritaceans. The ability to remodel the interior of the shell, developed primarily in gastropods with a non-nacreous shell structure, has contributed greatly to the acquisition of these antipredatory features.
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            Bangiomorpha pubescensn. gen., n. sp.: implications for the evolution of sex, multicellularity, and the Mesoproterozoic/Neoproterozoic radiation of eukaryotes

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              Calibrating the Cryogenian.

              The Neoproterozoic was an era of great environmental and biological change, but a paucity of direct and precise age constraints on strata from this time has prevented the complete integration of these records. We present four high-precision U-Pb ages for Neoproterozoic rocks in northwestern Canada that constrain large perturbations in the carbon cycle, a major diversification and depletion in the microfossil record, and the onset of the Sturtian glaciation. A volcanic tuff interbedded with Sturtian glacial deposits, dated at 716.5 million years ago, is synchronous with the age of the Franklin large igneous province and paleomagnetic poles that pin Laurentia to an equatorial position. Ice was therefore grounded below sea level at very low paleolatitudes, which implies that the Sturtian glaciation was global in extent.
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                Author and article information

                Journal
                Proc Biol Sci
                Proc. Biol. Sci
                RSPB
                royprsb
                Proceedings of the Royal Society B: Biological Sciences
                The Royal Society
                0962-8452
                1471-2954
                25 May 2016
                : 283
                : 1831
                : 20160221
                Affiliations
                Department of Earth Science, University of California at Santa Barbara , Santa Barbara, CA 93106, USA
                Author notes
                Author information
                http://orcid.org/0000-0002-4707-9428
                Article
                PMC4892792 PMC4892792 4892792 rspb20160221
                10.1098/rspb.2016.0221
                4892792
                27194696
                b48c9797-85fa-47a9-8ead-748e7c6577f9
                © 2016 The Author(s)

                Published by the Royal Society. All rights reserved.

                History
                : 31 January 2016
                : 25 April 2016
                Funding
                Funded by: National Science Foundation, http://dx.doi.org/10.13039/100000001;
                Award ID: EAR-0922305
                Funded by: Geological Society of America, http://dx.doi.org/10.13039/100005720;
                Award ID: W. Cole Storrs Memorial Research Fund
                Funded by: University of California, Santa Barbara, http://dx.doi.org/10.13039/100007183;
                Categories
                1001
                144
                Research Articles
                Custom metadata
                May 25, 2016

                drill holes,Neoproterozoic,Precambrian palaeontology,Vampyrellida,acritarch

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