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Benjamin Gill

Harvard University
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  • to Harvard Geobiology

    Hey all,

    The December issue of Geology had a little bit of everything for every shade of geobiologist. I linked the papers below.

    January 4, 2010
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  • to Harvard Geobiology

    ...and the last one, for the more paleontologically inclined, suggests that tommotiids (enigmatic Early Cambrian fossils) maybe a stem group of phoronids and/or brachiopods based on similarities in their shell microstructure.

    Happy New Year!

    Homologous skeletal secretion in tommotiids and brachiopods. Balthasar U. (2009) Geology.
    January 4, 2010
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  • to Harvard Geobiology

    For the more microbially inclined, this paper suggests strategies that halophilic Archaea may utilize to survive for long periods of time in pockets of fluid trapped in evaporite minerals.

    How do prokaryotes survive in fluid inclusions in halite for 30 k.y.?. Schubert B. A. (2009) Geology.
    January 4, 2010
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  • to Harvard Geobiology

    The second paper tries to link changes between the dominant marine carbonate mineralogies (i.e. aragonite and low-magnesium calcite) during the Phanerozoic to the inferred pCO2 of the atmosphere.

    Controls on carbonate skeletal mineralogy: Global CO2 evolution and mass extinctions. Zhuravlev A. Yu. (2009) Geology.
    January 4, 2010
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  • to Harvard Geobiology

    First one is by Justin Ries (now at UNC-Chapel Hill) concerning affects of acidification on a wide variety of calcifying organisms.

    Marine calcifiers exhibit mixed responses to CO2-induced ocean acidification. Ries J. B. (2009) Geology.
    January 4, 2010
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  • to Harvard Geobiology

    Hey everyone,

    Here is a new Science paper from my old lab group. It discusses the first known appearance of euxinia in the geological record and its relation to the evolution of the oxygenation of the ocean/atmosphere.

    A Late Archean Sulfidic Sea Stimulated by Early Oxidative Weathering of the Continents. Reinhard C. T. (2009) Science.
    October 30, 2009
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  • to Harvard Geobiology

    Hey all,
    Here's another stromatolite paper. This one is by a friend in my former lab at Riverside. It tries to show that stromatolites from the Gunflint and Biwabik iron formations were iron-oxidizing bacteria and not cyanobacteria using iron isotopes and rare earth elements.

    Iron-oxidizing microbial ecosystems thrived in late Paleoproterozoic redox-stratified oceans. Planavsky Noah (2009) Earth and Planetary Science Letters.
    September 24, 2009
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  • to Harvard Geobiology

    This article features new utility for rare sulfur and iron isotopes of pyrite: determining the source of detrital pyrites in two Archean successions. It also discusses the implications of the presence of detrital pyrite in samples on the secular trends in the rare sulfur isotope record of the Archean.

    Multiple sulphur and iron isotope composition of detrital pyrite in Archaean sedimentary rocks: A new tool for provenance analysis. Hofmann Axel (2009) Earth and Planetary Science Letters.
    September 18, 2009
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  • to Harvard Geobiology

    Along the lines of our discussion next Friday there is a new paper out in PPP discussing the Early Cambrian reefs in South China. Apparently the reefs on the Yangtze Platform were dominated by stromatolites and thrombolites.

    Early Cambrian microbial reefs, archaeocyathan inter-reef communities, and associated facies of the Yangtze Platform. Hicks Melissa (2009) Palaeogeography, Palaeoclimatology, Palaeoecology.
    September 12, 2009
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    September 9, 2009
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    September 9, 2009
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