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Long-Term Variability of Temperature and 14 C in the Gulf Stream

Oceanographic Implications

Bibliographic Data

ID9241783
AuthorsEllen M Druffel
Year1983
Volume25
Issue2
Pages449-458
Publication date1983-01-01
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0033822200005749
OpenAlexW262990472
LanguageEN
References cited14

Variability in temperature and 14 C levels are recorded in coralline aragonite that grew in the Gulf Stream during the past four centuries. In particular, 18 O/ 16 O ratios reflect a decrease of ca 1°C in surface water temperature during the latter part of the Little Ice age. 14 C levels also rose in the surface waters of the Gulf Stream and in atmospheric CO 2 during the Maunder minimum. These observations indicate that ocean circulation may have been significantly different in the North Atlantic around the beginning of the 18th century

Aragonite · Calcite · Climatology · Gulf Stream · Mineralogy · Ocean current · Radiocarbon dating · Sea surface temperature · Surface water · Coral and Marine Ecosystems Studies · Environmental Science · Isotope Analysis in Ecology · Marine and fisheries research · Geology · Oceanography · Paleontology

  • The Maunder Minimum

    Open Access•John A Eddy•Science•1976

  • Atmospheric14C changes resulting from fossil fuel CO2 release and cosmic ray flux variability

    Open Access•M Stuiver, Paul D Quay•Earth and Planetary Science Letters•1981

  • Lamont Radiocarbon Measurements VIII

    Open Access•Wallace S Broecker, Edwin A Olson•Radiocarbon•1961

  • Lamont Radiocarbon Measurements VI

    Open Access•Wallace S Broecker, Edwin A Olson•Radiocarbon•1959

  • The Radiocarbon Record in Tree Rings of the Last 8000 Years

    Open Access•Hans E Sueß•Radiocarbon•1980

  • Radiocarbon in Annual Coral Rings of Belize and Florida

    Open Access•Ellen M Druffel•Radiocarbon•1980

Highly citedNo

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