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      A key environmental driver of osteichthyan evolution and the fish-tetrapod transition?

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          Abstract

          Tides are a major component of the interaction between the marine and terrestrial environments, and thus play an important part in shaping the environmental context for the evolution of shallow marine and coastal organisms. Here, we use a dedicated tidal model and palaeogeographic reconstructions from the Late Silurian to early Late Devonian (420 Ma, 400 Ma and 380 Ma, Ma = millions of years ago) to explore the potential significance of tides for the evolution of osteichthyans (bony fish) and tetrapods (land vertebrates). The earliest members of the osteichthyan crown-group date to the Late Silurian, approximately 425 Ma, while the earliest evidence for tetrapods is provided by trackways from the Middle Devonian, dated to approximately 393 Ma, and the oldest tetrapod body fossils are Late Devonian, approximately 373 Ma. Large tidal ranges could have fostered both the evolution of air-breathing organs in osteichthyans to facilitate breathing in oxygen-depleted tidal pools, and the development of weight-bearing tetrapod limbs to aid navigation within the intertidal zones. We find that tidal ranges over 4 m were present around areas of evolutionary significance for the origin of osteichthyans and the fish-tetrapod transition, highlighting the possible importance of tidal dynamics as a driver for these evolutionary processes.

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          Efficient Inverse Modeling of Barotropic Ocean Tides

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            A chronology of Paleozoic sea-level changes.

            Sea levels have been determined for most of the Paleozoic Era (542 to 251 million years ago), but an integrated history of sea levels has remained unrealized. We reconstructed a history of sea-level fluctuations for the entire Paleozoic by using stratigraphic sections from pericratonic and cratonic basins. Evaluation of the timing and amplitude of individual sea-level events reveals that the magnitude of change is the most problematic to estimate accurately. The long-term sea level shows a gradual rise through the Cambrian, reaching a zenith in the Late Ordovician, then a short-lived but prominent withdrawal in response to Hirnantian glaciation. Subsequent but decreasingly substantial eustatic highs occurred in the mid-Silurian, near the Middle/Late Devonian boundary, and in the latest Carboniferous. Eustatic lows are recorded in the early Devonian, near the Mississippian/Pennsylvanian boundary, and in the Late Permian. One hundred and seventy-two eustatic events are documented for the Paleozoic, varying in magnitude from a few tens of meters to approximately 125 meters.
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              Global Sea Floor Topography from Satellite Altimetry and Ship Depth Soundings

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                Author and article information

                Contributors
                Journal
                Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
                Proc. R. Soc. A.
                The Royal Society
                1364-5021
                1471-2946
                October 2020
                October 21 2020
                October 2020
                : 476
                : 2242
                : 20200355
                Affiliations
                [1 ]School of Ocean Sciences, Bangor University, Menai Bridge, UK
                [2 ]Department of Organismal Biology, Uppsala University, Uppsala, Sweden
                [3 ]Department of Physics, University of Oxford, Oxford, UK
                Article
                10.1098/rspa.2020.0355
                03ac0f15-0ab7-4052-938b-03c6d5411818
                © 2020

                https://royalsociety.org/-/media/journals/author/Licence-to-Publish-20062019-final.pdf

                https://royalsociety.org/journals/ethics-policies/data-sharing-mining/

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