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Precise Temporal Correlation of Holocene Mollusk Shells Using Sclerochronology

Published online by Cambridge University Press:  20 January 2017

Thomas M. Marchitto Jr.,
Glenn A. Jones,
Glenn A. Goodfriend and
Christopher R. Weidman
Thomas M. Marchitto Jr.
Affiliation:
Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program in Oceanography, Woods Hole, Massachusetts 02543
Glenn A. Jones
Affiliation:
Texas Institute of Oceanography, Texas A&M University, Galveston, Texas 77553
Glenn A. Goodfriend
Affiliation:
Department of Geology, George Washington University, Washington, DC 20052
Christopher R. Weidman
Affiliation:
NOAA Northeast Center of National Marine Fisheries Service, Woods Hole, Massachusetts 02543
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Abstract

Annual growth bands of mollusk shells record several types of paleoenvironmental information, including geochemical proxies for water properties and morphological characteristics of growth and mortality. Sclerochronology, the marine counterpart of dendrochronology, offers a way to link individual shells together to form long continuous records of such parameters. It also allows for precise dating of recent shells and identification of contemporaneous fossil individuals. The longevity of the ocean quahog Arctica islandica (commonly >100 yr) makes this species well suited for sclerochronology. Band width records of contemporaneous A. islandica specimens from the same region exhibit high correlations (ρ = 0.60–0.80 for spans of ≥30 bands), indicating some common environmental influences on shell growth. By adopting several strict criteria, fossil (dead-collected) shells can be linked into composite sclerochronologies. A seven-shell 154-yr chronology was constructed for Georges Bank using three live-collected and four dead-collected shells. Band width matching indicates that the dead-collected individuals died in A.D. 1950, 1971, 1978, and 1989. Sclerochronological age assignments were verified using aspartic acid racemization dating. Construction of a 1000-yr sclerochronology is judged to be feasible using the described methods.

Information

Type
Research Article
Information
Quaternary Research , Volume 53 , Issue 2 , March 2000, pp. 236 - 246
Copyright
University of Washington

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References

Arthur, M.A., Williams, D.F., Jones, D.S., (1983). Seasonal temperature–salinity changes and the rmocline development in the mid-Atlantic Bight as recorded by the isotopic composition of bivalves.. Geology 11, 655–659.2.0.CO;2>CrossRefGoogle Scholar
Carter, J.G., (1980). Environmental and biological controls of bivalve shell mineralogy and microstructure.. Rhoads, D.C., Lutz, R.A., Skeletal Growth of Aquatic Organisms Plenum, New York.69–114.Google Scholar
Collines, M.J., Waite, E.R., van Duin, A.C.T., (1999). Predicting protein decomposition: The case of aspartic-acid racemization kinetics.. Jones, M.K., Molecular Information and Prehistory 51–64.Google Scholar
Cook, E.R., Briffa, K.R., Meko, D.M., Graybill, A., Funkhouser, G., (1995). The ‘segment length curse’ in long tree-ring chronology development for palaeoclimatic studies.. The Holocene 5, 229–237.Google Scholar
David, P., Delay, B., Berthou, P., Jarne, P., (1995). Alternative models for allozyme-associated heterosis in the marine bivalve Spisula ovalis.. Genetics 139, 1719–1726.CrossRefGoogle ScholarPubMed
Dettman, D.L., Lohmann, K.C., (1993). Seasonal change in Paleogene surface water δ18O: Fresh water bivalves of western North America.. Swart, P.K., Climate Change in Continental Isotopic Records: Geophysical Monograph 78 AGU, Washington.153–163.Google Scholar
Dickson, R., Lazier, J., Meincke, J., Rhines, P., Swift, J., (1996). Long-term coordinated changes in the convective activity of the North Atlantic.. Progress in Oceanography 38, 241–295.CrossRefGoogle Scholar
Druffel, E.M., (1989). Decadal time scale variability of ventilation in the North Atlantic: High-precision measurements of bomb radiocarbon in banded corals.. Journal of Geophysical Research 94, 3271–3285.CrossRefGoogle Scholar
Goodfriend, G.A., (1991). Patterns of racemization and epimerization of amino acids in land snail shells over the course of the Holocene.. Geochimica et Cosmochimica Acta 55, 293–302.CrossRefGoogle Scholar
Goodfriend, G.A., (1992). Rapid racemization of aspartic acid in mollusc shells and potential for dating over recent centuries.. Nature 357, 399–401.Google Scholar
Goodfriend, G.A., Rollins, H.B., (1998). Recent barrier beach retreat in Georgia: Dating exhumed salt marshes by aspartic acid racemization and post-bomb radiocarbon.. Journal of Coastal Research 14, 960–969.Google Scholar
Jones, D.S., (1980). Annual cycle of shell growth increment formation in two continental shelf bivalves and its paleoecologic significance.. Paleobiology 6, 331–340.CrossRefGoogle Scholar
Jones, D.S., (1981). Annual growth increments in shells of Spisula solidissima record marine temperature variability.. Science 211, 165–167.CrossRefGoogle ScholarPubMed
Jones, D.S., (1983). Sclerochronology: Reading the record of the molluscan shell.. American Scientist 71, 384–391.Google Scholar
Jones, D.S., Arthur, M.A., Allard, D.J., (1989). Sclerochronological records of temperature and growth from shells of Mercenaria mercenaria from Narragansett Bay, Rhode Island.. Marine Biology 102, 225–234.Google Scholar
Kennish, M.J., (1980). Shell microgrowth analysis: Mercenaria mercenaria as a type example for research in population dynamics.. Rhoads, D.C., Lutz, R.A., Skeletal Growth of Aquatic Organisms Plenum, New York.255–294.Google Scholar
Killingley, J.S., Berger, W.H., (1979). Stable isotopes in a mollusk shell: Detection of upwelling events.. Science 205, 186–188.CrossRefGoogle Scholar
Krantz, D.E., Williams, D.F., Jones, D.S., (1987). Ecological and paleoenvironmental information using stable isotope profiles from living and fossil molluscs.. Palaeogeography, Palaeoclimatology, Palaeoecology 58, 249–266.CrossRefGoogle Scholar
Lazzari, M. A., (1995)., Monthly and annual means of sea surface temperature, Boothbay Harbor, Maine, 1905 through 1994.. Research Document 95/1, Maine Dept. of Marine Resources. .Google Scholar
Lutz, R.A., Rhoads, D.C., (1980). Growth patterns within the molluscan shell: An overview.. Rhoads, D.C., Lutz, R.A., Skeletal Growth of Aquatic Organisms Plenum, New York.203–254.CrossRefGoogle Scholar
Murawski, S.A., Ropes, J.W., Serchuk, F.M., (1982). Growth of the ocean quahog, Arctica islandica, in the Middle Atlantic Bight.. Fishery Bulletin 80, 21–34.Google Scholar
Nicol, D., (1951). Recent species of the veneroid pelecypod Arctica.. Journal of the Washington Academy of Science 41, 102–106.Google Scholar
Reichart, G.-J., Horn, I., van der Laan, S.R., McDonough, W.F., Witbaard, R., (1998). Multi-year, intra-annual climate signals from trace element records of Quahog shells (Arctica islandica) by LA-ICP-MS.. Mineralogical Magazine 62A, 1243–1244.Google Scholar
Rhoads, D.C., Pannella, G., (1970). The use of molluscan shell growth patterns in ecology and paleoecology.. Lethaia 3, 143–161.CrossRefGoogle Scholar
Ropes, J.W., (1985). Modern methods to age oceanic bivalves.. Nautilus 99, 53–57.Google Scholar
SAS Institute Inc. (1990)., SAS Procedures Guide, Version 6, Third Edition,.. p, 224, SAS Institute Inc. Cary, NC.Google Scholar
Stuiver, M., Becker, B., (1993). High-precision decadal calibration of the radiocarbon time scale, AD 1950–6000 BC.. Radiocarbon 35, 35–65.CrossRefGoogle Scholar
Stuiver, M., Braziunas, T.F., (1993). Modeling atmospheric 14C influences and 14C ages of marine samples to 10,000 BC.. Radiocarbon 35, 137–189.CrossRefGoogle Scholar
Tevesz, M.J.S., (1972). Implications of absolute age and season of death data compiled for Recent Gemma gemma.. Lethaia 5, 31–38.Google Scholar
Thompson, I., Jones, D.S., Dreibelbis, D., (1980). Annual internal growth banding and life history of the ocean quahog Arctica islandica (Mollusca: Bivalvia).. Marine Biology 57, 25–34.Google Scholar
Weidman, C.R., (1995). Development and Application of the Mollusc Arctica islandica as a Paleoceanographic Tool for the North Atlantic Ocean.. MIT/WHOI Joint Program, .Google Scholar
Weidman, C.R., Jones, G.A., (1993). A shell-derived time history of bomb 14C on Georges Bank and its Labrador Sea implications.. Journal of Geophysical Research 98, 14,577–14,588.CrossRefGoogle Scholar
Weidman, C.R., Jones, G.A., (1993). Development of the mollusc Arctica islandica as a palaeoceanographic tool for reconstructing annual and seasonal records of Δ14C and δ18O in the mid-to-high latitude North Atlantic Ocean.. Isotope Techniques in the Study of Past and Current Environmental Changes in the Hydrosphere and the Atmosphere International Atomic Energy Agency, Vienna.p. 461–470.Google Scholar
Weidman, C.R., Jones, G.A., Lohmann, K.C., (1994). The long-lived mollusc Arctica islandica: A new paleoceanographic tool for the reconstruction of bottom temperatures for the continental shelves of the northern North Atlantic Ocean.. Journal of Geophysical Research 99, 18,305–18,314.CrossRefGoogle Scholar
Williams, D.F., Arthur, M.A., Jones, D.S., Healy-Williams, N., (1982). Seasonality and mean annual sea surface temperatures from isotopic and sclerochronological records.. Nature 296, 432–434.Google Scholar
Witbaard, R., Duineveld, G.C.A., (1990). Shell-growth of the bivalve Arctica islandica (L.), and its possible use for evaluating the status of the benthos in the subtidal North Sea.. Basteria 54, 63–74.Google Scholar