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      Deep-sea hydrothermal vents as natural egg-case incubators at the Galapagos Rift

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          Abstract

          The discovery of deep-sea hydrothermal vents in 1977 challenged our views of ecosystem functioning and yet, the research conducted at these extreme and logistically challenging environments still continues to reveal unique biological processes. Here, we report for the first time, a unique behavior where the deep-sea skate, Bathyraja spinosissima, appears to be actively using the elevated temperature of a hydrothermal vent environment to naturally “incubate” developing egg-cases. We hypothesize that this behavior is directly targeted to accelerate embryo development time given that deep-sea skates have some of the longest egg incubation times reported for the animal kingdom. Similar egg incubating behavior, where eggs are incubated in volcanically heated nesting grounds, have been recorded in Cretaceous sauropod dinosaurs and the rare avian megapode. To our knowledge, this is the first time incubating behavior using a volcanic source is recorded for the marine environment.

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          Most cited references31

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          Submarine thermal sprirngs on the galapagos rift.

          The submarine hydrothermal activity on and near the Galápagos Rift has been explored with the aid of the deep submersible Alvin. Analyses of water samples from hydrothermal vents reveal that hydrothermal activity provides significant or dominant sources and sinks for several components of seawater; studies of conductive and convective heat transfer suggest that two-thirds of the heat lost from new oceanic lithosphere at the Galápagos Rift in the first million years may be vented from thermal springs, predominantly along the axial ridge within the rift valley. The vent areas are populated by animal communities. They appear to utilize chemosynthesis by sulfur-oxidizing bacteria to derive their entire energy supply from reactions between the seawater and the rocks at high temperatures, rather than photosynthesis.
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            Hydrothermal vents and the origin of life.

            Submarine hydrothermal vents are geochemically reactive habitats that harbour rich microbial communities. There are striking parallels between the chemistry of the H(2)-CO(2) redox couple that is present in hydrothermal systems and the core energy metabolic reactions of some modern prokaryotic autotrophs. The biochemistry of these autotrophs might, in turn, harbour clues about the kinds of reactions that initiated the chemistry of life. Hydrothermal vents thus unite microbiology and geology to breathe new life into research into one of biology's most important questions - what is the origin of life?
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              Universal primer cocktails for fish DNA barcoding

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                Author and article information

                Contributors
                Pelayo.salinas@fcdarwin.org.ec
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                8 February 2018
                8 February 2018
                2018
                : 8
                : 1788
                Affiliations
                [1 ]Charles Darwin Research Station, Av Charles Darwin s/n, Puerto Ayora, Santa Cruz, Galapagos Islands Ecuador
                [2 ]Galapagos Marine Research and Exploration (GMaRE), joint CDF-ESPOL research program, Charles Darwin Research Station, Santa Cruz, Galapagos Islands Ecuador
                [3 ]ISNI 0000 0001 2216 0097, GRID grid.422252.1, Pristine Seas, , National Geographic Society, ; Washington, D. C. USA
                [4 ]ISNI 000000041936754X, GRID grid.38142.3c, Harvard Microrobotics Laboratory, , Harvard University, ; Cambridge, MA USA
                [5 ]ISNI 0000 0004 0416 2242, GRID grid.20431.34, Department of Ocean Engineering, , University of Rhode Island, ; Narragansett, RI 02882 USA
                [6 ]ISNI 0000 0001 0806 2909, GRID grid.253561.6, Pacific Shark Research Center, Moss Landing Marine Laboratories, 8272 Moss Landing Rd, ; Moss, CA 95039 USA
                [7 ]Department of Ichthyology, California Academy of Sciences, 55 Music Concourse Drive, San Francisco, CA 94118 USA
                [8 ]South African Institute for Aquatic Biodiversity, Private Bag 1015, Grahamstown, 6140 South Africa
                [9 ]ISNI 0000 0001 2168 8324, GRID grid.261241.2, Save Our Seas Shark Research Center and Guy Harvey Research Institute, , Nova Southeastern University, 8000 N Ocean Drive, ; Dania Beach, FL 33004 USA
                [10 ]ISNI 0000 0001 2097 4281, GRID grid.29857.31, Department of Biology, , Pennsylvania State University, University Park, ; State College, PA 16802 USA
                [11 ]ISNI 0000 0004 1936 9297, GRID grid.5491.9, Ocean and Earth Science, , University of Southampton, Waterfront Campus, ; Southampton, SO14 3ZH UK
                [12 ]Marine Geoscience, National Oceanography Centre, European Way, Southampton, SO14 3ZH UK UK
                Author information
                http://orcid.org/0000-0003-4361-6529
                http://orcid.org/0000-0003-4604-8192
                Article
                20046
                10.1038/s41598-018-20046-4
                5805729
                29422624
                bd03bc15-a3c3-47ce-9978-702f1d38c50b
                © The Author(s) 2018

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 21 September 2017
                : 10 January 2018
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