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Volumn 303, Issue 5655, 2004, Pages 202-207

14C Activity and Global Carbon Cycle Changes over the Past 50,000 Years

Author keywords

[No Author keywords available]

Indexed keywords

CALIBRATION; CARBON; GEOMAGNETISM; GLACIERS; ICE; RADIOMETRY; SEDIMENTS;

EID: 0346340053     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.1090300     Document Type: Article
Times cited : (402)

References (43)
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    • 14C decay constant, and t is the calendar age (37).
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    • Materials and methods are available as supporting material on Science Online.
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    • note
    • 14C for the past 50 ka B.P. within ±10%. of the simple box model. Subsequent gracial perturbation experiments were carried out in the box model as a computational expedient.
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    • note
    • 2 by an average of -0.3‰ (41).
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    • Reduced deep-ocean ventilation is consistent with potentially restricted NADW formation and penetration in the glacial ocean. Global transects of radio-carbon distribution in the oceans suggest that NADW formation is responsible for sequestering up to 75% of the radiocarbon in the deep ocean (42).
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    • This change represents a 120-m lowering of sea level and the resultant shift of carbonate sedimentation off the continental shelves into deep water, where dissolution is much more extensive. Discussion and details of the glacial carbon cycle boundary conditions are summarized in SOM Text, fig. S3, and table S2.
  • 43
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    • note
    • This work was supported by NSF (OCE-0117356), Lawrence Livermore National Laboratory (LDRD-97-ERI-009), and the U.S. Department of Energy (W-7405-Eng-48). We thank the ODP Core Repository in Bremen for core sampling; B. Frantz and P. Zermeno for sample preparation assistance; C. Laj, M. Frank, J.-P. Valet, and J. Stoner for providing their data of past geomagentic field intensities; and S. Johnsen for making available the revised GRIPss09sea chronology. This is WHOI contribution no, 11061.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.