Open-File and Technical Reports

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This section includes two Open File reports for the U.S. Geological Survey documenting amino acid racemization research on the U.S. Pacific coast (Wehmiller et al.,1977a and 1977b), Gomez Pit research by June Mirecki (1985, 1990) and Lamothe et al. (1995), database research by Vincent Pellerito (2004), a compilation of racemization data from sites in Florida (Wehmiller and colleagues, unpublished), and a technical report regarding studies of the organic geochemistry of Delaware Bay sediments (Wehmiller and Lethen, 1975).


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Now showing 1 - 5 of 10
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    Uranium-series coral ages from the US Atlantic Coastal Plain–the ‘‘80 ka problem’’ revisited
    (Department of Geology and College of Marine Studies, University of Delaware, Newark, 2004) Wehmiller, John F.; Simmons, Kathleen R.; Cheng, Hai; Edwards, R. Lawrence; Martin-McNaughton, Jamie; York, Linda L.; Krantz, David E.; Shen, Chuan-Chou
    Uranium series coral ages for emergent units from the passive continental margin US Atlantic Coastal Plain (ACP) suggest sea level above present levels at the end of marine oxygen isotope stage (MIS) 5, contradicting age-elevation relations based on marine isotopic or coral reef models of ice equivalent sea level. We have reexamined this problem by obtaining high precision Th-230/U-238 and Pa-231/U-235 thermal ionization mass spectrometric ages for recently collected and carefully cleaned ACP corals, many in situ. We recognize samples that show no evidence for diagenesis on the basis of uranium isotopic composition and age concordance. Combining new and earlier data, among those ages close to or within the age range of MIS 5, over 85% cluster between 65 and 85 ka BP. Of the corals that we have analyzed, those that show the least evidence for diagenesis on the basis of uranium isotopic composition and age concordance have ages between 80 and 85 ka BP, consistent with a MIS 5a correlation. The units from which these samples have been collected are all emergent and have elevations within B3–5m of those few units where early stage 5 (B125,000 ka BP) coral ages have been obtained. The ACP appears to record an unusual history of relative sea level throughout MIS 5, a history that is also apparent in the dated coral record for Bermuda. We speculate that this history is related to the regional (near-to intermediate-field) effects of ancestral Laurentide Ice sheets on last interglacial shorelines of the western North Atlantic.
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    The Pleistocene Planktonic Foraminiferal Aminostratigraphy of Ocean Drilling Program Hole 625B in the Northeast Gulf of Mexico
    (University of Delaware, Newark., 1990) Johnson, Beverly J.
    Amino acid analyses were performed on four planktonic species of foraminifera and a mixed foraminiferal species assemblage through the Quaternary section of Ocean Drilling Program Site 625B in the northeast Gulf of Mexico. The extent of isoleucine epimerization in the individual species increased with time as the overall rate of epimerization decreased with time. Extents of epimerization among the species in increasing order are Globigerinoides ruber, Orbulina universa, Neogloboquadrina dutertrei and the Globorotalia tumida-menardii complex. The mixed foraminiferal species assemblage was found to epimerize at a rate intermediate to the limits delineated by Globigerinoides ruber and the Globorotalia tumida-menardii complex.
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    Aminostratigraphy, geochronology and geochemistry of fossils from Late Cenozoic marine units in southeastern Virginia
    (University of Delaware, Newark, 1990) Mirecki, June
    Paired Amino Acid Racemization (AAR) and Electron Spin Resonance (ESR) data have been obtained from individual mollusc valves (g. Mercenaria) collected from stratified nearshore deposits at three sites in southeastern Virginia (Gomez Pit, Norris Bridge and Yadkin Pit). AAR and ESR data are used here to define aminozones in the region, and to infer age relationships among these superposed aminozones. These data are compared to U-Th analyses of corals from both sites (Szabo, 1985). Age differences among aminozones are estimated using models of racemization kinetics. Previous workers have generally concluded that the lithologic section at Gomez Pit represents a single transgression followed by minor regression. However, AAR and ESR data indicate at least one unconformity in this transgressive sequence, representing approximately 100 ka. The uppermost aminozone lla is defined by a mean ALLO/ISO values of 0.141+/-0.026 (n = 55). Aminozone lla directly overlies aminozone llc (ALLO/ISO = 0.335+/-0.028; n = 19). Molluscs representing a third, lowest aminozone (lld; ALLO/ISO = 0.471+/-0.038; n = 9) are recognized, but taphonomic and ESR data suggest that lld molluscs in Gomez Pit may be reworked. At Norris Bridge, only aminozone lld (ALLO/ISO = 0.473+/-0.020; n = 5) is recognized. ESR age estimates for aminozone lla range from 93-125 ka (n = 4), in general agreement with a Stage 5 estimate of 75+/-5 ka from U-Th analyses of corals from the same unit. ESR age estimates of 220 and 262 ka were calculated from 2 shells showing ALLO/ISO = 0.33; these data support a Stage 7 or Stage 9 interpretation for aminozone llc. AAR kinetic models suggest an age $>$400 ka for aminozone lld shells, inconsistent with a 187+/-20 ka age from a solitary coral at Norris Bridge. Attempts to obtain age estimates using ESR have been unsuccessful. Shells representing excellent, good, fair and poor preservation conditions from Gomez Pit aminozone lla were compared to determine the effects of condition on precision of amino acid data. These data were used to test the hypothesis that leaching by groundwater selectively removes the most extensively epimerized (free) amino acids from the mollusc shell, thus lowering the ALLO/ISO value. No statistically significant difference in amino acid concentrations, amino acid fractions or ALLO/ISO values was found among these Gomez Pit shells representing different preservation characteristics.
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    Amino acid racemization dating of some coastal plain sites, southeastern Virginia and northeastern North Carolina
    (University of Delaware, Newark, DE, 1985) Mirecki, June
    Bivalve mollusks (g. Mercenaria and g. Anadara) have been analyzed from 4 southeastern coastal plain sites using the amino acid racemization (AAR) technique for correlation and age estimate purposes. As seen previously (Wehmiller and Belknap, 1982), a conflict exists between age estimates obtained by AAR and V-series methods at the Norris Bridge, VA locality. Here, V-series dating of coral yields a 187 ±20 KA age, while AAR methods suggest a 400 to 500 KA age. The following methods are employed to understand this discrepancy at the Norris Bridge site: 1). Analysis of standard samples to ensure uniform sample preparation and system operation; 2). Quantification of variation in Mercenari'a and Anadara samples for each field site; 3). Qualitative comparison of AAR behavior between Mercenaria and Anadara to assess suitability of Anadara for dating purposes; 4). Aminostratigraphic correlation of field sites using both genera, and 5). Estimation of AAR ages using the the non-linear model of Wehmiller and Belknap (1982). Standard samples analyzed for this study show relatively good preCISIon. Coefficients of variation (CVs) of D/L leucine values are 5.7% (ILC-A) and 9.1% (ILC-B). Overall, both ILC-A and -B show accuracy within 6% when compared to other University of Delaware analyses. Several valves of each genus were analyzed from all sites to determine field site precision. CVs for multiple Mercenaria samples from each site are as follows: Gomez Pit, VA (5.2%); New Light Pit, VA (7.0%); Moyock Pit, N.C. (8.8%) and Norris Bridge, VA (4.4%). CVs for Anadara samples are slightly higher, but comparable for each field site. No Anadara were analyzed from the New Light Pit locality. On the basis of an identical order of racemization rates (i.e. ASP2:ALA> LEU>VAL) and similar ASP/LEU values in both genera, Mercenaria and Anadara qualitatively show similar racemization behavior. 3 clusters of DjL leucine values have been discerned from these field site analyses. These D/L leucine values are used to correlate fossiliferous strata in the southeastern Virginia and northeastern North Carolina Using the non-linear kinetic model, these Coastal Plain. D/L values suggest the following ages: 0.21 to 0.25 (75 KA) and 0.530 (approximately 400 KA). D/L values ranging between 0.33 and 0.38 are tentatively estimated to be 100 to 200 KA in age.
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    Comparison of approaches to dating Atlantic coastal plain sediments, Virginia Beach, Virginia
    (Washington, DC : U.S. Nuclear Regulatory Commission, 1998-03) Lamothe, Michel; Wehmiller, John F.; Noller, Jay S.