منابع مشابه
Model simulation of mid-cretaceous ocean circulation.
tween Eurasia and Africa that result in a primary eastward-directed, low-velocity current flow along the mid-Cretaceous Eurasian, northern Tethys margin. This conclusion appears to be at odds with sedimentologic and paleontologic field evidence (2, 3) obtained from the Helvetic tectonic unit that is exposed in the northern Alps and represents the former northern Tethys margin in southern Europe...
متن کاملHadley circulation shrinkage in the mid-Cretaceous
H. Hasegawa, R. Tada, X. Jiang, Y. Suganuma, S. Imsamut, P. Charusiri, N. Ichinnorov, and Y. Khand Department of Earth and Planetary Science, the University of Tokyo, Tokyo, Japan Chengdu Institute of Geology and Mineral Resources, Chengdu, China National Institute of Polar Research, Tokyo, Japan Department of Mineral Resources, Bureau of Geological Survey, Bangkok, Thailand Department of Geolo...
متن کاملModel simulation of the cretaceous ocean circulation.
Three-dimensional numerical ocean circulation model experiments that were designed to evaluate the circulation characteristics for the mid-Cretaceous ( approximately 100 million years ago) show that the primary direction of flow through the Tethys Ocean was eastward; in contrast, a westward flowing circumglobal Tethys current has been a consistent feature of earlier reconstructions of Cretaceou...
متن کاملSimulation of modern and middle Cretaceous marine dO with an ocean-atmosphere general circulation model
[1] We have developed a coupled ocean-atmosphere general circulation model, the GENESIS-MOM model, with the ability to transport and fractionate water isotopes in the ocean and atmosphere. The model is used to predict modern and Cretaceous precipitation and seawater dO. The model reproduces the large-scale modernday isotopic distribution. In the zonal mean, the difference between simulated and ...
متن کاملEvidence for thermohaline-circulation reversals controlled by sea-level change in the latest Cretaceous
During the early Maastrichtian (ca. 71 Ma), important changes occurred in climate, weathering, sea level, biota, and the global carbon cycle. Global climate was characterized by rapid cooling within the long-term post-Santonian refrigeration of high-latitude surface and intermediate waters (Barrera, 1994; Huber et al., 1995). The intensity of continental weathering increased, as inferred from t...
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ژورنال
عنوان ژورنال: Nature Geoscience
سال: 2012
ISSN: 1752-0894,1752-0908
DOI: 10.1038/ngeo1444