Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Houben, Alexander J.P."'
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 1 March 2021 565
Autor:
Gallagher, Stephen J., Wade, Bridget, Qianyu, Li, Holdgate, Guy R., Bown, Paul, Korasidis, Vera A., Scher, Howie, Houben, Alexander J.P., McGowran, Brian, Allan, Tony
Publikováno v:
In Global and Planetary Change August 2020 191
Autor:
Houben, Alexander J.P., van Mourik, Caroline A., Montanari, Alessandro, Coccioni, Rodolfo, Brinkhuis, Henk
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 1 June 2012 335-336:75-83
Publikováno v:
In Review of Palaeobotany and Palynology 2011 165(3):175-182
Autor:
Pross, Jörg, Houben, Alexander J.P., van Simaeys, Stefaan, Williams, Graham L., Kotthoff, Ulrich, Coccioni, Rodolfo, Wilpshaar, Martin, Brinkhuis, Henk
Publikováno v:
In Review of Palaeobotany and Palynology 2010 158(3):213-235
Autor:
Cramwinckel, Margot J., Coxall, Helen K., Śliwińska, Kasia K., Polling, Marcel, Harper, Dustin T., Bijl, Peter K., Brinkhuis, Henk, Eldrett, James S., Houben, Alexander J.P., Peterse, Francien, Schouten, Stefan, Reichart, Gert Jan, Zachos, James C., Sluijs, Appy, Marine palynology and palaeoceanography, Organic geochemistry, Stratigraphy and paleontology, Marine Palynology
Publikováno v:
Paleoceanography and Paleoclimatology
Paleoceanography and Paleoclimatology, 35(10). Wiley Online Library
Paleoceanography and Paleoclimatology, 35(10). Wiley Online Library
Several studies indicate that North Atlantic Deep Water (NADW) formation might have initiated during the globally warm Eocene (56–34 Ma). However, constraints on Eocene surface ocean conditions in source regions presently conducive to deep water fo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::78c7a4eb057a9aa75257575ab2d00c28
https://dspace.library.uu.nl/handle/1874/409605
https://dspace.library.uu.nl/handle/1874/409605
Autor:
Houben, Alexander J.P., Quaijtaal, Willemijn, Wade, Bridget S., Schouten, Stefan, Brinkhuis, Henk, Organic geochemistry, Marine palynology and palaeoceanography, Marine Palynology
Publikováno v:
Newsletters on Stratigraphy, 52(2), 131. Gebruder Borntraeger Verlagsbuchhandlung
The Eocene – Oligocene Transition (EOT, ~34–33.5 Ma) marks a major transition in Cenozoic climate evolution through the relatively rapid establishment of a continental-scale ice sheet on Antarctica. The EOT is characterized by two ~200 kyr spaced
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=narcis______::2208b346fc1d6c3b2cab2d255d7461b3
https://dspace.library.uu.nl/handle/1874/390061
https://dspace.library.uu.nl/handle/1874/390061
Autor:
Hartman, Julian D., Sangiorgi, Francesca, Salabarnada, Ariadna, Peterse, Francien, Houben, Alexander J.P., Schouten, Stefan, Brinkhuis, Henk, Escutia, Carlota, Bijl, Peter K., Marine palynology and palaeoceanography, Organic geochemistry, Marine Palynology
Publikováno v:
Climate of the Past, 14(9), 1275. European Geosciences Union
The volume of the Antarctic continental ice sheet(s) varied substantially during the Oligocene and Miocene ( ∼ 34-5Ma) from smaller to substantially larger than today, both on million-year and on orbital timescales. However, reproduction through ph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=narcis______::05e7cb9a95153348ebfef545aa384845
https://dspace.library.uu.nl/handle/1874/372566
https://dspace.library.uu.nl/handle/1874/372566
Autor:
Bijl, Peter K., Houben, Alexander J.P., Hartman, Julian D., Pross, Jörg, Salabarnada, Ariadna, Escutia, Carlota, Sangiorgi, Francesca, Marine palynology and palaeoceanography, Marine Palynology
Publikováno v:
Climate of the Past, Vol 14, Pp 1015-1033 (2018)
Climate of the Past, 14(7), 1015. European Geosciences Union
Digital.CSIC. Repositorio Institucional del CSIC
instname
Climate of the Past, 14(7), 1015. European Geosciences Union
Digital.CSIC. Repositorio Institucional del CSIC
instname
Next to atmospheric CO concentrations, ice-proximal oceanographic conditions are a critical factor for the stability of Antarctic marine-terminating ice sheets. The Oligocene and Miocene epochs (∼ 34-5 Myr ago) were time intervals with atmospheric
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8d3e9cefdf00e82fa1ebe331bbf76e79
https://dspace.library.uu.nl/handle/1874/366653
https://dspace.library.uu.nl/handle/1874/366653
Autor:
Bijl, Peter K., Houben, Alexander J.P., Bruls, Anja, Pross, Jörg, Sangiorgi, Francesca, Marine palynology and palaeoceanography, Marine Palynology
Publikováno v:
Journal of Micropalaeontology, 1, 37, 105-138
Journal of Micropalaeontology, 37(1), 105. Geological Society of London
Journal of Micropalaeontology, 37(1), 105. Geological Society of London
There is growing interest in the scientific community in reconstructing the paleoceanography of the Southern Ocean during the Oligocene–Miocene because these time intervals experienced atmospheric CO2 concentrations with relevance to our future. Ho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::587bd1b84cde921c353b916f4d24ba3b
http://resolver.tudelft.nl/uuid:ea8605c1-3687-47ee-b983-8bbb3d80e529
http://resolver.tudelft.nl/uuid:ea8605c1-3687-47ee-b983-8bbb3d80e529