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δ13C as an Indicator of Palaeoenvironments
2001Reconstruction of ancient climates (palaeoclimates) is a major goal in areas of the Earth sciences seeking insight into the history of the Earth. On the one hand a petroleum organic geochemist is able to use such information to provide valuable insight on palaeoclimatic and palaeoenvironmental conditions likely to generate rocks offering good sources ...
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Early Cretaceous insect faunas and palaeoenvironment
Cretaceous Research, 1995Abstract The record of Cretaceous insect life has increased dramatically in the last few decades. A new family database suggests that a peak of diversity was reached in the Early Cretaceous, the biggest in the Phanerozoic prior to the Tertiary. The subsequent decline is attributable to the rapid replacement of older floras by angiosperms.
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Late Cainozoic palaeoenvironments of southern Africa
2020Pollen bearing deposits of the southwestern Cape have been studied. In the oldest sections of the cores different types of Tertiary vegetation are represented since the Late Oligocene or Early Miocene until their ultimate extinction. The sporomorphae of the younger parts of the deposits are typical of the type of vegetation which exists in these ...
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Loess and Palaeoenvironments across Eurasia
Quaternary International, 2006A.A. Velichko, A.E. Dodonov, N.R. Catto
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