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  • American Association for the Advancement of Science (AAAS)  (2)
  • 1
    Publication Date: 2008-06-28
    Description: Samples from a 1.76-kilometer-deep corehole drilled near the center of the late Eocene Chesapeake Bay impact structure (Virginia, USA) reveal its geologic, hydrologic, and biologic history. We conducted stratigraphic and petrologic analyses of the cores to elucidate the timing and results of impact-melt creation and distribution, transient-cavity collapse, and ocean-water resurge. Comparison of post-impact sedimentary sequences inside and outside the structure indicates that compaction of the crater fill influenced long-term sedimentation patterns in the mid-Atlantic region. Salty connate water of the target remains in the crater fill today, where it poses a potential threat to the regional groundwater resource. Observed depth variations in microbial abundance indicate a complex history of impact-related thermal sterilization and habitat modification, and subsequent post-impact repopulation.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Gohn, G S -- Koeberl, C -- Miller, K G -- Reimold, W U -- Browning, J V -- Cockell, C S -- Horton, J W Jr -- Kenkmann, T -- Kulpecz, A A -- Powars, D S -- Sanford, W E -- Voytek, M A -- New York, N.Y. -- Science. 2008 Jun 27;320(5884):1740-5. doi: 10.1126/science.1158708.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉U.S. Geological Survey, Reston, VA 20192, USA. ggohn@usgs.gov〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18583604" target="_blank"〉PubMed〈/a〉
    Keywords: Bacteria/growth & development/*isolation & purification ; *Ecosystem ; Geologic Sediments/chemistry/*microbiology ; Hot Temperature ; Salinity ; Seawater ; Time ; Virginia
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2005-11-29
    Description: We review Phanerozoic sea-level changes [543 million years ago (Ma) to the present] on various time scales and present a new sea-level record for the past 100 million years (My). Long-term sea level peaked at 100 +/- 50 meters during the Cretaceous, implying that ocean-crust production rates were much lower than previously inferred. Sea level mirrors oxygen isotope variations, reflecting ice-volume change on the 10(4)- to 10(6)-year scale, but a link between oxygen isotope and sea level on the 10(7)-year scale must be due to temperature changes that we attribute to tectonically controlled carbon dioxide variations. Sea-level change has influenced phytoplankton evolution, ocean chemistry, and the loci of carbonate, organic carbon, and siliciclastic sediment burial. Over the past 100 My, sea-level changes reflect global climate evolution from a time of ephemeral Antarctic ice sheets (100 to 33 Ma), through a time of large ice sheets primarily in Antarctica (33 to 2.5 Ma), to a world with large Antarctic and large, variable Northern Hemisphere ice sheets (2.5 Ma to the present).〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Miller, Kenneth G -- Kominz, Michelle A -- Browning, James V -- Wright, James D -- Mountain, Gregory S -- Katz, Miriam E -- Sugarman, Peter J -- Cramer, Benjamin S -- Christie-Blick, Nicholas -- Pekar, Stephen F -- New York, N.Y. -- Science. 2005 Nov 25;310(5752):1293-8.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Geological Sciences, Rutgers University, Piscataway, NJ 08854, USA. kgm@rci.rutgers.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/16311326" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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