hdl:10013/epic.37876
publisher:10.1016/j.epsl.2010.07.026
Modeling the influence of a reduced equator-to-pole sea surface temperature gradient on the distribution of water isotopes in the Early/Middle Eocene
Speelman, E. N., Sewall, J. O., Noone, D., Huber, M., von der Heydt, A., Sinninghe Damsté, J. and Reichart, Gert-Jan
;
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Jelle.Bijma [ at ] awi.de
Abstract
Item Type
Article
Authors
Speelman, E. N., Sewall, J. O., Noone, D., Huber, M., von der Heydt, A., Sinninghe Damsté, J. and Reichart, Gert-Jan
;
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Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past > WP 3.3: Proxy Development and Innovation: the Baseline for Progress in Paleoclimate Research
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past > WP 3.3: Proxy Development and Innovation: the Baseline for Progress in Paleoclimate Research
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Published
Eprint ID
24736
DOI
10.1016/j.epsl.2010.07.026
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Cite as
Speelman, E. N.
,
Sewall, J. O.
,
Noone, D.
,
Huber, M.
,
von der Heydt, A.
,
Sinninghe Damsté, J.
and
Reichart, G. J.
(2010):
Modeling the influence of a reduced equator-to-pole sea surface temperature gradient on the distribution of water isotopes in the Early/Middle Eocene
,
Earth and Planetary Science Letters,
298
(1),
pp. 57-65
.
doi: 10.1016/j.epsl.2010.07.026
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