Zobrazeno 1 - 10
of 56
pro vyhledávání: '"C. A. Hollis"'
Autor:
C. J. Hollis, S. Naeher, C. D. Clowes, B. D. A. Naafs, R. D. Pancost, K. W. R. Taylor, J. Dahl, X. Li, G. T. Ventura, R. Sykes
Publikováno v:
Climate of the Past, Vol 18, Pp 1295-1320 (2022)
Late Paleocene deposition of an organic-rich sedimentary facies on the continental shelf and slope of New Zealand and eastern Australia has been linked to short-lived climatic cooling and terrestrial denudation following sea leve
Externí odkaz:
https://doaj.org/article/f3e4419e18354e1b910b1f0a1402743f
Autor:
D. J. Lunt, F. Bragg, W.-L. Chan, D. K. Hutchinson, J.-B. Ladant, P. Morozova, I. Niezgodzki, S. Steinig, Z. Zhang, J. Zhu, A. Abe-Ouchi, E. Anagnostou, A. M. de Boer, H. K. Coxall, Y. Donnadieu, G. Foster, G. N. Inglis, G. Knorr, P. M. Langebroek, C. H. Lear, G. Lohmann, C. J. Poulsen, P. Sepulchre, J. E. Tierney, P. J. Valdes, E. M. Volodin, T. Dunkley Jones, C. J. Hollis, M. Huber, B. L. Otto-Bliesner
Publikováno v:
Climate of the Past, Vol 17, Pp 203-227 (2021)
We present results from an ensemble of eight climate models, each of which has carried out simulations of the early Eocene climate optimum (EECO, ∼ 50 million years ago). These simulations have been carried out in the framework of the Deep-Time Mod
Externí odkaz:
https://doaj.org/article/7b6841f438e54b4f9d2617c7b44cdd2b
Autor:
G. N. Inglis, F. Bragg, N. J. Burls, M. J. Cramwinckel, D. Evans, G. L. Foster, M. Huber, D. J. Lunt, N. Siler, S. Steinig, J. E. Tierney, R. Wilkinson, E. Anagnostou, A. M. de Boer, T. Dunkley Jones, K. M. Edgar, C. J. Hollis, D. K. Hutchinson, R. D. Pancost
Publikováno v:
Climate of the Past, Vol 16, Pp 1953-1968 (2020)
Accurate estimates of past global mean surface temperature (GMST) help to contextualise future climate change and are required to estimate the sensitivity of the climate system to CO2 forcing through Earth's history. Previous GMST estimates for the l
Externí odkaz:
https://doaj.org/article/a6015aacaf1c444ea1e0ec384a95fb96
Autor:
C. J. Hollis, T. Dunkley Jones, E. Anagnostou, P. K. Bijl, M. J. Cramwinckel, Y. Cui, G. R. Dickens, K. M. Edgar, Y. Eley, D. Evans, G. L. Foster, J. Frieling, G. N. Inglis, E. M. Kennedy, R. Kozdon, V. Lauretano, C. H. Lear, K. Littler, L. Lourens, A. N. Meckler, B. D. A. Naafs, H. Pälike, R. D. Pancost, P. N. Pearson, U. Röhl, D. L. Royer, U. Salzmann, B. A. Schubert, H. Seebeck, A. Sluijs, R. P. Speijer, P. Stassen, J. Tierney, A. Tripati, B. Wade, T. Westerhold, C. Witkowski, J. C. Zachos, Y. G. Zhang, M. Huber, D. J. Lunt
Publikováno v:
Geoscientific Model Development, Vol 12, Pp 3149-3206 (2019)
The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time that Earth's atmospheric CO2 concentrations exceeded 1000 ppm. Global mean temperatures were also substantially warmer than those of the present day. As suc
Externí odkaz:
https://doaj.org/article/2c9cbda7c2704c4da455998fb6fc0496
Autor:
D. J. Lunt, M. Huber, E. Anagnostou, M. L. J. Baatsen, R. Caballero, R. DeConto, H. A. Dijkstra, Y. Donnadieu, D. Evans, R. Feng, G. L. Foster, E. Gasson, A. S. von der Heydt, C. J. Hollis, G. N. Inglis, S. M. Jones, J. Kiehl, S. Kirtland Turner, R. L. Korty, R. Kozdon, S. Krishnan, J.-B. Ladant, P. Langebroek, C. H. Lear, A. N. LeGrande, K. Littler, P. Markwick, B. Otto-Bliesner, P. Pearson, C. J. Poulsen, U. Salzmann, C. Shields, K. Snell, M. Stärz, J. Super, C. Tabor, J. E. Tierney, G. J. L. Tourte, A. Tripati, G. R. Upchurch, B. S. Wade, S. L. Wing, A. M. E. Winguth, N. M. Wright, J. C. Zachos, R. E. Zeebe
Publikováno v:
Geoscientific Model Development, Vol 10, Iss 2, Pp 889-901 (2017)
Past warm periods provide an opportunity to evaluate climate models under extreme forcing scenarios, in particular high ( > 800 ppmv) atmospheric CO2 concentrations. Although a post hoc intercomparison of Eocene ( ∼ 50 Ma) climate model simulations
Externí odkaz:
https://doaj.org/article/f7eaea5171304bb78e8d55e7d251702b
Autor:
K. M. Pascher, C. J. Hollis, S. M. Bohaty, G. Cortese, R. M. McKay, H. Seebeck, N. Suzuki, K. Chiba
Publikováno v:
Climate of the Past, Vol 11, Iss 12, Pp 1599-1620 (2015)
The long-term cooling trend from middle to late Eocene was punctuated by several large-scale climate perturbations that culminated in a shift to "icehouse" climates at the Eocene–Oligocene transition. We present radiolarian micro-fossil assemblage
Externí odkaz:
https://doaj.org/article/6ecf4a35ba80443ca609765dd85edfef
Autor:
C. J. Hollis, B. R. Hines, K. Littler, V. Villasante-Marcos, D. K. Kulhanek, C. P. Strong, J. C. Zachos, S. M. Eggins, L. Northcote, A. Phillips
Publikováno v:
Climate of the Past, Vol 11, Iss 7, Pp 1009-1025 (2015)
Re-examination of sediment cores from Deep Sea Drilling Project (DSDP) Site 277 on the western margin of the Campbell Plateau (paleolatitude of ~65° S) has identified an intact Paleocene–Eocene (P–E) boundary overlain by a 34 cm thick record of
Externí odkaz:
https://doaj.org/article/828178611f194d2ab3138194c74ae60b
Autor:
S. J. Gallagher, N. Exon, M. Seton, M. Ikehara, C. J. Hollis, R. Arculus, S. D'Hondt, C. Foster, M. Gurnis, J. P. Kennett, R. McKay, A. Malakoff, J. Mori, K. Takai, L. Wallace
Publikováno v:
Scientific Drilling, Vol 17, Pp 45-50 (2014)
A major International Ocean Discovery Program (IODP) workshop covering scientific ocean drilling in the southwest Pacific Ocean was held in Sydney, Australia, in late 2012. The workshop covered all fields of geoscience, and drilling targets in the ar
Externí odkaz:
https://doaj.org/article/bdd2ce1ca54e4fdcb88aa86520f5f293
Publikováno v:
Micropaleontology. 54:41-48
The timing of the origin of the Southern Ocean is important for studies of Antarctic biologic evolution and for understanding past climate change. The long standing theory that separation of Australia from Antarctica at the end of the Eocene allowed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b78da4ea12c4d9df5d028906225a0e57
https://doi.org/10.47894/mpal.54.1.05
https://doi.org/10.47894/mpal.54.1.05
Publikováno v:
Journal of Applied Chemistry. 2:501-510
Experimental methods are described for the evaluation of the important mechanical properties of (a) hard plastics, (b) elastomers, when only small amounts of the materials are available. For thermoplastics of type (a), the impact strength was determi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4893559ec0b50f10b6e5a3f70791ffea
https://doi.org/10.1002/jctb.5010020902
https://doi.org/10.1002/jctb.5010020902