How To Use Paleocene In A Sentence
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Mid-Cretaceous faulting is observed along the Ran ridge, whereas the axis of the Paleocene rifted zone is shifted slightly further to the west in the Voring margin.
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In the Mesozoic, and into the Paleocene, limestone and dolomite interbedded with shale, clay and anhydrite prevailed in a more restricted, shallow marine to lagoonal environment.
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In the Mesozoic, and into the Paleocene, limestone and dolomite interbedded with shale, clay and anhydrite prevailed in a more restricted, shallow marine to lagoonal environment.
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Both polar and Tethyan dispersal routes have been well documented for Cretaceous and Paleocene decapod crustaceans.
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Before and after the late Paleocene thermal maximum, upwelling and biological productivity were less intense, and seafloor dysoxia was restricted to neritic parts of the basin.
Bürger and Cubasch: Are multiproxy climate reconstructions robust? « Climate Audit
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At present, the oldest reliable fossil from this family is a tarsometatarsus that was found in Colorado, dating back to the Paleocene epoch.
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The current study reports on new neoplagiaulacid multituberculates from the Paleocene Paskapoo Formation of central Alberta, Canada, at localities along the Blindman River near the City of Red Deer.
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Paleocene faunas were dominated by what we refer to as archaic mammals: condylarths (archaic ungulates), archaic primates, small rodent-like multituberculates, pantodonts, and others.
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Terrestrial deposits contain fossils ranging from Paleocene leaf imprints to Cretaceous dinosaur remains.
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During the Paleocene, almost all of the decapod occurrences were in fine siliciclastic sediments.
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This trend is evident at a coarse scale in a comparison of the combined rarefaction curves for sites from the uppermost 15 m of the Cretaceous against all Paleocene sites.
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Fossils of volant paleoganthous carinate birds from the Paleocene and Eocene appear phenetically most similar to tinamiform birds.
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During the late Cretaceous and early Paleocene periods plant-eating mammals were frugivores, presumably because fruit can be more easily processed than foliage.
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This pattern was documented for both bivalves and gastropods and continued from the mid to late Paleocene until the early Eocene.
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The first cycle initiated in the early Paleocene and represents a transition from Cretaceous marine turbidites and shales to subaerial fluvial sandstones and conglomerates.
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Echinoids are among the most conspicuous and diverse constituents of the Upper Cretaceous and Paleocene marine invertebrate fauna of Argentina.
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Paleocene and Eocene sediments were deposited on a polygenetic sub-Paleogene surface.
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Paleocene faunas were dominated by what we refer to as archaic mammals: condylarths (archaic ungulates), archaic primates, small rodent-like multituberculates, pantodonts, and others.
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Archaic ungulates (‘condylarths’) were long known to be among many eutherians to make their first appearance and proliferate in the Paleocene.
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Currano and her colleagues found that during the comparatively cooler end of the Paleocene epoch, 15 to 38 percent of leaves showed insect damage.
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Present along the surface exposures of the anticline are rocks dating from Upper Cretaceous to Paleocene age.
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In the north Gjallar Ridge, fault patterns above the dome suggest activity before Paleocene time.
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Particularly important for British landscape development was rifting of the Greenland-European plate in the early Paleocene.
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The first cycle initiated in the early Paleocene and represents a transition from Cretaceous marine turbidites and shales to subaerial fluvial sandstones and conglomerates.
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Some mammal teeth from the Paleocene of France show characters of both bats and insectivores (the group including the hedgehogs, shrews and moles of today).
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Paleocene fossil outcrops abound in the glauconite rich gray clay substrata of the creek banks exposed beneath the deep rich surface soils.
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Fossils of volant paleoganthous carinate birds from the Paleocene and Eocene appear phenetically most similar to tinamiform birds.
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During the late Paleocene thermal maximum, the upwelling of low-oxygen intermediate Tethyan water into the epicontinental basin led to enhanced biological productivity and anoxia at the seafloor.
Bürger and Cubasch: Are multiproxy climate reconstructions robust? « Climate Audit
