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Volumn 122, Issue 1, 2000, Pages 23-

The responses of the terrestrial carbon cycle to global change across the Paleocene/Eocene boundary

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Indexed keywords


EID: 0343433781     PISSN: 11035897     EISSN: 20000863     Source Type: Journal    
DOI: 10.1080/11035890001221023     Document Type: Article
Times cited : (1)

References (3)
  • 2
    • 0029529085 scopus 로고
    • Dissociation of oceanic methane hydrate as a cause of carbon isotope excursion at the end of the Paleocene
    • Dickens, G.R., O’Neil, J.R., Rea, D.K. & Owen, R.M., 1995: Dissociation of oceanic methane hydrate as a cause of carbon isotope excursion at the end of the Paleocene. Paleoceanography 10, 965-971.
    • (1995) Paleoceanography , vol.10 , pp. 965-971
    • Dickens, G.R.1    O’Neil, J.R.2    Rea, D.K.3    Owen, R.M.4
  • 3
    • 0030758008 scopus 로고    scopus 로고
    • A blast of gas in the latest Paleocene: Simulating first-order effects of massive dissociation of organic methane hydrate
    • Dickens, G.R., Castillo, M.M. & Walker, J.C.G., 1998: A blast of gas in the latest Paleocene: simulating first-order effects of massive dissociation of organic methane hydrate. Geology 25, 259-262.
    • (1998) Geology , vol.25 , pp. 259-262
    • Dickens, G.R.1    Castillo, M.M.2    Walker, J.C.G.3


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.