메뉴 건너뛰기




Volumn 316, Issue 5830, 2007, Pages 1456-1459

Marine radiocarbon evidence for the mechanism of deglacial atmospheric CO2 rise

Author keywords

[No Author keywords available]

Indexed keywords

CARBON 14; CARBON DIOXIDE; SEA WATER; SURFACE WATER;

EID: 34250220033     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1138679     Document Type: Article
Times cited : (243)

References (42)
  • 2
    • 0346340053 scopus 로고    scopus 로고
    • K. Hughen et al., Science 303, 202 (2004).
    • (2004) Science , vol.303 , pp. 202
    • Hughen, K.1
  • 6
    • 0035808596 scopus 로고    scopus 로고
    • E. Monnin et al., Science 291, 112 (2001).
    • (2001) Science , vol.291 , pp. 112
    • Monnin, E.1
  • 11
    • 3142697010 scopus 로고    scopus 로고
    • J. D. Ortiz et al., Geology 32, 521 (2004).
    • (2004) Geology , vol.32 , pp. 521
    • Ortiz, J.D.1
  • 13
    • 0035861526 scopus 로고    scopus 로고
    • Y. J. Wang et al., Science 294, 2345 (2001).
    • (2001) Science , vol.294 , pp. 2345
    • Wang, Y.J.1
  • 16
    • 34250217730 scopus 로고    scopus 로고
    • 14C values calculated with the original GISP2 chronology (15) and compare them to the original Cariaco record (2), based on correlation to GISP2 (fig. 53).
    • 14C values calculated with the original GISP2 chronology (15) and compare them to the original Cariaco record (2), based on correlation to GISP2 (fig. 53).
  • 18
    • 0003220740 scopus 로고
    • GEOSECS Atlantic, Pacific and Indian Ocean Expeditions
    • U.S. Government Printing Office, Washington, DC
    • G. Ostlund, H. Craig, W. S. Broecker, D. Spencer, GEOSECS Atlantic, Pacific and Indian Ocean Expeditions, vol. 7, Sharebased Data and Graphics (U.S. Government Printing Office, Washington, DC, 1987).
    • (1987) Sharebased Data and Graphics , vol.7
    • Ostlund, G.1    Craig, H.2    Broecker, W.S.3    Spencer, D.4
  • 19
    • 34250157697 scopus 로고    scopus 로고
    • 14C values with respect to the contemporaneous atmosphere, rather than calculating ventilation ages by decay projection (39) because of large uncertainties in initial surface-ocean reservoir ages and the possibility of multiple intermediate- and deep-water sources with different ventilation histories.
    • 14C values with respect to the contemporaneous atmosphere, rather than calculating ventilation ages by decay projection (39) because of large uncertainties in initial surface-ocean reservoir ages and the possibility of multiple intermediate- and deep-water sources with different ventilation histories.
  • 21
    • 34250176844 scopus 로고    scopus 로고
    • 2.
    • 2.
  • 29
    • 18644383641 scopus 로고    scopus 로고
    • S. L. Jaccard et al., Science 308, 1003 (2005).
    • (2005) Science , vol.308 , pp. 1003
    • Jaccard, S.L.1
  • 38
    • 28544453427 scopus 로고    scopus 로고
    • L. F. Robinson et al., Science 310, 1469 (2005).
    • (2005) Science , vol.310 , pp. 1469
    • Robinson, L.F.1
  • 40
    • 8444249640 scopus 로고    scopus 로고
    • W. Broecker et al., Science 306, 1169 (2004).
    • (2004) Science , vol.306 , pp. 1169
    • Broecker, W.1
  • 42
    • 34250218881 scopus 로고    scopus 로고
    • 14C measurement; and T. Blunier for providing Dome C EDC 3 time scale and for valuable discussions on synchronization of the different ice cores. This manuscript was improved by comments from R. Keeling and two anonymous reviewers. Support was provided by NSF grants OCE-9809026 and OCE-0214221.
    • 14C measurement; and T. Blunier for providing Dome C EDC 3 time scale and for valuable discussions on synchronization of the different ice cores. This manuscript was improved by comments from R. Keeling and two anonymous reviewers. Support was provided by NSF grants OCE-9809026 and OCE-0214221.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.