Results 181 to 190 of about 16,983 (236)

Metal-driven anaerobic oxidation of methane and the Sturtian deglaciation. [PDF]

Nat Commun
Hu J, Li S, Wang SJ, Peckmann J, Guan H, Jiang SY, Chen W, Cui H, Qin Z, Liu P, Suo Y, Jiang Z, Li D, Wang N, Li X, Zhong Y, Li R, Yang XM, Konhauser KO.   +18 more
europepmc   +1 more source

Postglacial ecosystem development of a hydrothermal landscape in Yellowstone National Park. [PDF]

Proc Natl Acad Sci U S A
Whitlock C, Schiller CM, Hostetler SW, Hurwitz S, Alt M, Brown SR, Harrison LN, Alder JR, Busch K, Shelly J, McWethy DB.   +10 more
europepmc   +1 more source

Mid Holocene rapid thinning and rethickening of the East Antarctic ice sheet suggested by glacial isostatic adjustment. [PDF]

Sci Rep
Okuno J, Hattori A, Doi K, Aoyama Y, Fukuda Y.   +4 more
europepmc   +1 more source

Mismatch in reindeer resilience to past and future warming signals ongoing declines. [PDF]

Sci Adv
Canteri E, Brown SC, Post E, Schmidt NM, Nogues-Bravo D, Fordham DA.   +5 more
europepmc   +1 more source

Toward the snowball earth deglaciation…

Climate Dynamics, 2010
The current state of knowledge suggests that the Neoproterozoic snowball Earth is far from deglaciation even at 0.2 bars of CO2. Since understanding the termination of the fully ice-covered state is essential to sustain, or not, the snowball Earth theory, we used an Atmospheric General Climate Model (AGCM) to explore some key factors which could induce
Gilles Ramstein, Gerhard Krinner, Guillaume le Hir   +2 more
exaly   +5 more sources

Deglaciation of Fennoscandia [PDF]

Quaternary Science Reviews, 2016
To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we have compiled and synthesized published geomorphological data for eskers, ice-marginal formations, lineations, marginal meltwater channels, striae, ice-dammed lakes, and ...
J M Harbor, Jakob Heyman, Arjen Stroeven   +2 more
exaly   +7 more sources

The sea-level fingerprint of a Snowball Earth deglaciation

Earth and Planetary Science Letters, 2014
Cap dolostones are thought to represent deposition from seas transgressing over formerly glaciated continental margins during Marinoan Snowball deglaciation.
Jerry Mitrovica, Jessica Creveling
exaly   +1 more source

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Early Deglaciation of the Labrador Shelf

Science, 1978
Two marine sediment cores from a basin on the southeastern Labrador Shelf penetrate a mud sequence extending back to 21,000 carbon-14 years before the present (B.P.). The benthic foraminifera are dominated by subartic nearshore species indicative of ice-free summer waters.
G, Vilks, P J, Mudie
openaire   +2 more sources

The deglacial hemicycle

Geologische Rundschau, 1964
Absolute age relationships between (a) size reduction of continental ice sheets, (b) glacio-eustatic sea level rise, (c) temperature changes of the ocean surface, and (d) temperature changes on land show that the proper sequence is as follows: first, withdrawal of the ice sheets; second, warming of the land surface; and, third, warming of the ocean ...
openaire   +1 more source