Pliocene - Middle Pleistocene biostratigraphy in the Central Danish North Sea wells E-1, P-1 and TWB-12
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چکیده
منابع مشابه
Microfaunal remains at Middle Pleistocene Qesem Cave, Israel: Preliminary results on small vertebrates, environment and biostratigraphy.
Preliminary results of the investigation of the microfauna at the Acheulo-Yabrudian Middle Pleistocene site of Qesem Cave, Israel, are presented. Thus far the assemblage includes ca. 10,000 bone and tooth fragments, of which 50% could be identified to the generic and some hundreds to the species level. Based on the current material, the fauna includes the following squamate reptiles: Laudakia s...
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چکیده ندارد.
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Over the last 5 million years, the global climate system has evolved toward a colder mean state, marked by large-amplitude oscillations in continental ice volume. Equatorward expansion of polar waters and strengthening temperature gradients have been detected. However, the response of the mid latitudes and high latitudes of the Southern Hemisphere is not well documented, despite the potential i...
متن کاملDeep-sea temperature and ice volume changes across the Pliocene-Pleistocene climate transitions.
Earth has undergone profound changes since the late Pliocene, which led to the development [approximately 2.7 million years ago (Ma)] and intensification (approximately 0.9 Ma) of large-scale Northern Hemisphere ice sheets, recorded as transitions in the benthic foraminiferal oxygen isotope (delta18Ob) record. Here we present an orbitally resolved record of deep ocean temperature derived from b...
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Background and objectives The primary objective of drilling at Site U1345 was to study high-resolution HoloceneLate Pleistocene paleoceanography at a proximal gateway location to the Arctic Ocean at a water depth of ~1008 m. The drill site is located on an interfluve ridge near the large and broad head of Navarin Submarine Channel off the Bering Sea Shelf. It is anticipated to receive ample sup...
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ژورنال
عنوان ژورنال: Danmarks Geologiske Undersøgelse Serie C
سال: 1995
ISSN: 2597-2995,0900-6362
DOI: 10.34194/seriec.v13.7117