Titlebook: Cenozoic Plants and Climates of the Arctic; Michael C. Boulter,Helen C. Fisher Conference proceedings 1994 Springer-Verlag Berlin Heidelbe

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Dinoflagellate Cysts and Climate Change through the Neogene fossilisable cysts is a major factor in how cyst data are interpreted. In addition, little is known of the natural occurrence of cysts in the plankton or their pathways through the water column before their final incorporation in bottom sediments. The distribution of cysts in bottom sediments is su

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Late Cretaceous Arctic Platanoids and High Latitude Climatecian and the end of the Cretaceous account for a peak of diversity and abundance of platanoids in the Anadyr-Koryak subregion of northeastern Russia. In the Cenomanian and again in the Santonian — Early Campanian there was a repeated occurrence of warmer and relatively drier climates which resulted

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Early Tertiary Vegetation of Arctic Canada and Its Relevance to Paleoclimatic Interpretationensitive animals indicate that severe frost never occurred, even during the long, dark winter. Cold month mean temperatures of 0–4 °C, warm month mean of >25 °C, and mean annual temperature of 12–15 °C are estimated. These estimates are higher than those derived from physiognomic analogy, probably b

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Alaskan Palaeogene Climates as Inferred from the Clamp Databasen critical levels are emphasized by these analyses. Any fossil leaf sample of woody dicotyledons can be analysed in the CLAMP database and various palaeoclimatic parameters estimated..The sequence of leaf assemblages on the Yakutat block, which is now at lat. 60° N at the head of the Gulf of Alaska,

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Invasion of Arcto-Tertiary Elements in the Palaeogene of Central Europefrom Central Europe (according to results of recent studies of . and other taxa). Some of these ‘pioneer forms’ (.) demonstrate a transition from azonal to zonal distributions in the subsequent periods.

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Romilda Mazzotta,Giovanni Bronzettirmation, may have affected the global environment. 2) Emplacement of extrusive complexes during break-up, which combined with a segmented plate boundary, controlled circulation of Paleogene waters in the Norwegian-Greenland Sea. This led to late Paleocene-early Eocene shallow basins with poor region

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