paleocene oor Nederlands
paleocene
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Paleocene
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(geology) Of or pertaining to a geologic epoch within the Paleogene period from about 65 to 56 million years ago; marked by the rise of the first large mammals in a tropical climate.
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Voorbeelde moet herlaai word.
This group was deposited during the early Paleocene epoch and is subdivided into two formations: the Houthem Formation (lower) and the Opglabbeek Formation (upper).
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The Landen Formation lies normally on top of a nonconformity with the Dutch Chalk Group, which is usually represented by the early Paleocene Houthem Formation.
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The Heers Formation is almost everywhere overlain by the Hannut Formation (clay, sand and limestone from the late Paleocene).
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The Ieper Group lies stratigraphically on top of the Landen Group (upper Paleocene) and below the Zenne Group (like the Ieper Group early Eocene in age).
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The thermal maximum caused a great extinction which is used to distinguish the Eocene fauna from that of the Paleocene.
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Other similar basal primates were widespread in Eurasia and Africa during the tropical conditions of the Paleocene and Eocene.
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All of these units are marine sands and clay cats from the Ypresian (55.8 - 48.6 million years ago) and Lutetian (48.6 - 40.4 million years ago) ages, when the eustatic sea level was relatively high after the Paleocene–Eocene Thermal Maximum.
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Because of the climatic conditions of the Paleocene, reptiles were more widely distributed over the globe than at present.
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To put this in perspective, this is about 200 times the background rate of degassing for the rest of the Paleocene.
Van South Haven naar Heartland in twee dagenWikiMatrix WikiMatrix
The group consists of two formations of Thanetian (late Paleocene) to Ypresian (early Eocene) age.
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Paleocene and later plant fossils are generally attributed to modern genera or to closely related taxa.
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The Landen Formation consists of shallow marine and lagoonal sediments (mostly clay, sandy clay and marl) from the late Paleocene to early Eocene (between 58 and 54 million years old).
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The formation consists of calcareous sandstone and was formed about 60 million years ago, in the Paleocene epoch.
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From the beginning of this period, the temperature of the planet rose in one of the quickest (in geological terms) and most extreme episodes of global warming in the geological record, termed Paleocene–Eocene Thermal Maximum.
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The earliest proboscids, the African Eritherium and Phosphatherium of the late Paleocene, heralded the first radiation.
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Approximately 60% of late-Cretaceous Scleractinia coral genera failed to cross the K–Pg boundary into the Paleocene.
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Zonation based on time series for the Paleocene Aquifer System (SS_1000) with indication of piezometers and their respective trend.
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During the Paleocene, the continents continued to drift toward their present positions.
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From the beginning of this period, the temperature of the planet rose in one of the quickest (in geological terms) and most extreme episodes of global warming in the geological record, termed Paleocene–Eocene Thermal Maximum.
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In the process, the core of the Alps, with the terranes that were subducted in the Paleocene and Eocene, still moves upward.
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Gastornis is an extinct genus of large flightless birds that lived during the late Paleocene and Eocene epochs of the Cenozoic era.
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MO/36/011: Mammalian evolution and migration during the Paleocene-Eocene transition (60 to 50 million years ago) in the Northern Hemisphere
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Along the banks of the Potomac River are various types of fossils can be found from the Aquia Formation from the Paleocene, part of the Paleogene.
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Interestingly, there is a unique collection of Paleocene vertebrates from Central Africa in the federal heritage resulting from Belgian expeditions of the Royal Museum for Central Africa by Edmond Dartevelle in the Democratic Republic of Congo and Angola.
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The Paleocene is divided into three stages, the Danian, the Selandian and the Thanetian, as shown in the table above.
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34 sinne gevind in 10 ms. Hulle kom uit baie bronne en word nie nagegaan nie.