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Steven L Goldstein

Biographic Data

ID5597507
NAMESteven L Goldstein
GIVEN NAMESSteven L
FAMILY NAMEGoldstein
SIGNATUREGOLDSTEIN S L
VERIFIEDNo
TOTAL WORKS4
TOTAL CITATIONS5
AUTHOR COUNT4
EDITOR COUNT0
FIRST PUBLICATION YEAR2000
LATEST PUBLICATION YEAR2017
H-INDEX2
  • Radiocarbon Chronology of the DSDDP Core at the Deepest Floor of the Dead Sea

    Open Access•Hiroyuki Kitagawa, Mordechai Stein et al.•ARTICLE•Radiocarbon•2017•References: 43

    This study establishes the chronological framework of the sedimentary sequence deposited Dead Sea, ICDP 5017-1, Radiocarbon chronology during the past 50 ka at the deepest part of the Dead Sea (the ICDP 5017-1 site), which was recovered by the Dead Sea Deep Drilling Project (DSDDP) under the auspices of the International Continental Scientific Drilling Program (ICDP). The age-depth model is constructed using 38 14 C dates of terrestrial plant rem…

  • Radiocarbon Reservoir Ages as Freshwater-Brine Monitors in Lake Lisan, Dead Sea System

    Open Access•Mordechai Stein, Boaz Lazar et al.•ARTICLE•Radiocarbon•2013•Cited by: 2•References: 20

    A continuous and high-resolution record of the radiocarbon reservoir age (RA) has been recovered from the primary aragonites that were deposited from the last glacial Lake Lisan. The RA is calculated as the difference between the measured 14 C “apparent” age in the aragonite and the atmospheric age at any particular time. The RA shows temporal decreases during the time interval of ≃28 to ≃18 ka cal BP. This behavior is attributed to a continuous …

  • Reconstructing low levels of Lake Lisan by correlating fan-delta and lacustrine deposits

    Open Access•Malka Machlus, Yehouda Enzel et al.•ARTICLE•Quaternary International•2000

  • Radiocarbon Calibration Beyond the Dendrochronology Range

    Open Access•Mordechai Stein, Steven L Goldstein et al.•ARTICLE•Radiocarbon•2000•Cited by: 3•References: 29

    The radiocarbon timescale has been calibrated by dendrochronology back to 11.8 ka cal BP, and extended to 14.8 ka cal BP using laminated marine sediments from the Cariaco Basin. Extension to nearly 23.5 ka cal BP is based on comparison between 14 C and U-Th ages of corals. Recently, attempts to further extend the calibration curve to >40 kyr are based on laminated sediments from Lake Suigetsu, Japan, foraminifera in North Atlantic sediments, Sout…

  • Radiocarbon Calibration Beyond the Dendrochronology Range

    Open Access•Mordechai Stein, Steven L Goldstein et al.•ARTICLE•Radiocarbon•2000•Cited by: 3•References: 29

    The radiocarbon timescale has been calibrated by dendrochronology back to 11.8 ka cal BP, and extended to 14.8 ka cal BP using laminated marine sediments from the Cariaco Basin. Extension to nearly 23.5 ka cal BP is based on comparison between 14 C and U-Th ages of corals. Recently, attempts to further extend the calibration curve to >40 kyr are based on laminated sediments from Lake Suigetsu, Japan, foraminifera in North Atlantic sediments, Sout…

  • Radiocarbon Reservoir Ages as Freshwater-Brine Monitors in Lake Lisan, Dead Sea System

    Open Access•Mordechai Stein, Boaz Lazar et al.•ARTICLE•Radiocarbon•2013•Cited by: 2•References: 20

    A continuous and high-resolution record of the radiocarbon reservoir age (RA) has been recovered from the primary aragonites that were deposited from the last glacial Lake Lisan. The RA is calculated as the difference between the measured 14 C “apparent” age in the aragonite and the atmospheric age at any particular time. The RA shows temporal decreases during the time interval of ≃28 to ≃18 ka cal BP. This behavior is attributed to a continuous …

  • Reconstructing low levels of Lake Lisan by correlating fan-delta and lacustrine deposits

    Open Access•Malka Machlus, Yehouda Enzel et al.•ARTICLE•Quaternary International•2000

  • Radiocarbon Calibration Beyond the Dendrochronology Range

    Open Access•Mordechai Stein, Steven L Goldstein et al.•ARTICLE•Radiocarbon•2000•Cited by: 3•References: 29

    The radiocarbon timescale has been calibrated by dendrochronology back to 11.8 ka cal BP, and extended to 14.8 ka cal BP using laminated marine sediments from the Cariaco Basin. Extension to nearly 23.5 ka cal BP is based on comparison between 14 C and U-Th ages of corals. Recently, attempts to further extend the calibration curve to >40 kyr are based on laminated sediments from Lake Suigetsu, Japan, foraminifera in North Atlantic sediments, Sout…

  • Radiocarbon Reservoir Ages as Freshwater-Brine Monitors in Lake Lisan, Dead Sea System

    Open Access•Mordechai Stein, Boaz Lazar et al.•ARTICLE•Radiocarbon•2013•Cited by: 2•References: 20

    A continuous and high-resolution record of the radiocarbon reservoir age (RA) has been recovered from the primary aragonites that were deposited from the last glacial Lake Lisan. The RA is calculated as the difference between the measured 14 C “apparent” age in the aragonite and the atmospheric age at any particular time. The RA shows temporal decreases during the time interval of ≃28 to ≃18 ka cal BP. This behavior is attributed to a continuous …

  • Radiocarbon Chronology of the DSDDP Core at the Deepest Floor of the Dead Sea

    Open Access•Hiroyuki Kitagawa, Mordechai Stein et al.•ARTICLE•Radiocarbon•2017•References: 43

    This study establishes the chronological framework of the sedimentary sequence deposited Dead Sea, ICDP 5017-1, Radiocarbon chronology during the past 50 ka at the deepest part of the Dead Sea (the ICDP 5017-1 site), which was recovered by the Dead Sea Deep Drilling Project (DSDDP) under the auspices of the International Continental Scientific Drilling Program (ICDP). The age-depth model is constructed using 38 14 C dates of terrestrial plant rem…

Geology (4 works) · Geology and Paleoclimatology Research (4 works) · Oceanography (4 works) · Paleontology (4 works) · Holocene (3 works) · Marine and environmental studies (3 works) · Radiocarbon dating (3 works) · Aragonite (2 works) · Archaeology (2 works) · Archaeology and ancient environmental studies (2 works)

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