Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Hayden TG"'
Autor:
Cook, CP, Van De Flierdt, T, Williams, T, Hemming, SR, Iwai, M, Kobayashi, M, Jimenez-Espejo, FJ, Escutia, C, González, JJ, Khim, BK, McKay, RM, Passchier, S, Bohaty, SM, Riesselman, CR, Tauxe, L, Sugisaki, S, Galindo, AL, Patterson, MO, Sangiorgi, F, Pierce, EL, Brinkhuis, H, Klaus, A, Fehr, A, Bendle, JAP, Bijl, PK, Carr, SA, Dunbar, RB, Flores, JA, Hayden, TG, Katsuki, K, Kong, GS, Nakai, M, Olney, MP, Pekar, SF, Pross, J, Röhl, U, Sakai, T, Shrivastava, PK, Stickley, CE, Tuo, S, Welsh, K, Yamane, M
Publikováno v:
Cook, CP; Van De Flierdt, T; Williams, T; Hemming, SR; Iwai, M; Kobayashi, M; et al.(2013). Dynamic behaviour of the East Antarctic ice sheet during Pliocene warmth. Nature Geoscience, 6(9), 765-769. doi: 10.1038/ngeo1889. UC San Diego: Retrieved from: http://www.escholarship.org/uc/item/7cq9w66z
Warm intervals within the Pliocene epoch (5.33-2.58 million years ago) were characterized by global temperatures comparable to those predicted for the end of this century and atmospheric CO 2 concentrations similar to today. Estimates for global sea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______325::8fc3dd1e641c946725b0fb3a98eaae7a
http://www.escholarship.org/uc/item/7cq9w66z
http://www.escholarship.org/uc/item/7cq9w66z
Autor:
Houben AJ; Department of Earth Sciences, Laboratory of Palaeobotany and Palynology, Faculty of Geosciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, Netherlands. Alexander.Houben@TNO.nl, Bijl PK, Pross J, Bohaty SM, Passchier S, Stickley CE, Röhl U, Sugisaki S, Tauxe L, van de Flierdt T, Olney M, Sangiorgi F, Sluijs A, Escutia C, Brinkhuis H, Dotti CE, Klaus A, Fehr A, Williams T, Bendle JA, Carr SA, Dunbar RB, Flores JA, Gonzàlez JJ, Hayden TG, Iwai M, Jimenez-Espejo FJ, Katsuki K, Kong GS, McKay RM, Nakai M, Pekar SF, Riesselman C, Sakai T, Salzmann U, Shrivastava PK, Tuo S, Welsh K, Yamane M
Publikováno v:
Science (New York, N.Y.) [Science] 2013 Apr 19; Vol. 340 (6130), pp. 341-4.
