SFX by Ex Libris Inc.

Source:	Glacial‐Marine Sedimentation [0-87590-706-7; 1-118-66767-0] Anderson, John
yr:1989 -127S.

Basic

Sorry, no full text available...

Please use the document delivery service (see below)

Document delivery

Request document via Library/Bibliothek

Citation information

Check Google Book Search

Users interested in this article also expressed an interest in the following:
description	1.	Heinze, M. "Ocean biogeochemistry in the warm climate of the late Paleocene." Climate of the past 11.1 (2015): 63-79.
description	2.	Meissner, K. J. J. "The Paleocene-Eocene Thermal Maximum: How much carbon is enough?" Paleoceanography 29.10 (2014): 946-963.
description	3.	"Fifty million years ago." American scientist 78.1 (1990): 30-.
description	4.	Panchuk, K. "Sedimentary response to Paleocene-Eocene Thermal Maximum carbon release: A model-data comparison." Geology 36.4 (2008): 315-318.
description	5.	Ragueneau, O. "A review of the Si cycle in the modern ocean: Recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy." Global and planetary change 26.4 (2000): 317-365.
description	6.	Pagani, M. "Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum." Nature 442.7103 (2006): 671-675.
description	7.	Sluijs, A. "Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximum." Nature 441.7093 (2006): 610-613.
description	8.	Treguer, P. "Silica and the cycle of carbon in the ocean." Comptes rendus. Géoscience 334.1 (2002): 3-11.
description	9.	Storey, M. "Paleocene-Eocene Thermal Maximum and the Opening of the Northeast Atlantic." Science 316.5824 (2007): 587-589.
description	10.	Zachos, J. "Carbon dioxide forcing alone insufficient to explain Palaeocene-Eocene Thermal Maximum warming." Nature geoscience 2.8 (2009): 576-580.
description	11.	Nelson, David M. M. "Production and dissolution of biogenic silica in the ocean: Revised global estimates, comparison with regional data and relationship to biogenic sedimentation." Global biogeochemical cycles 9.3 (1995): 359-372.
description	12.	Ravizza, G. "An osmium isotope excursion associated with the late Paleocene thermal maximum: Evidence of intensified chemical weathering." Paleoceanography 16.2 (2001): 155-163.
description	13.	Kring, B. "Global Warming Special." Onearth 27.3 (2005): 20-37.
description	14.	Nunes, Flavia, F. "Abrupt reversal in ocean overturning during the Palaeocene/Eocene warm period." Nature 439.7072 (2006): 60-63.
description	15.	Jouzel, J. "Stable Carbon Cycle-Climate Relationship During the Late Pleistocene." Science 310.5752: 1313-7.
description	16.	Deprez, A. "Differential response at the seafloor during Palaeocene and Eocene ocean warming events at Walvis Ridge, Atlantic Ocean ( ODP Site 1262)." TERRA nova 29.1 (2017): 71-76.
description	17.	Meissner, Katrin J. "The importance of the terrestrial weathering feedback for multimillennial coral reef habitat recovery." Global biogeochemical cycles 26.3 (2012).
description	18.	Schubert, Brian A. "Reconciliation of marine and terrestrial carbon isotope excursions based on changing atmospheric CO2 levels." Nature communications 4.April (2013): 1653-1653.
description	19.	Yamaguchi, T. "Dwarfing of ostracodes during the Paleocene–Eocene Thermal Maximum at DSDP Site 401 (Bay of Biscay, North Atlantic) and its implication for changes in organic carbon cycle in deep-sea benthic ecosystem." Palaeogeography, palaeoclimatology, palaeoecology 346-347 (2012): 130-144.
description	20.	McInerney, Francesca A. "The paleocene-eocene thermal maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future." Annual review of earth and planetary sciences 39.1 (2011): 489-516.