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Cenozoic Plants and Climates of the Arctic Book

Cenozoic Plants and Climates of the Arctic
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Cenozoic Plants and Climates of the Arctic, Fifty million years ago, the Arctic Ocean was a warm sea, bounded by lush vegetation of the warm-temperate shores of Scandinavia, Siberia, Alaska and the Northwest Territories. Wind and storms were rare because Atlantic weather systems had not developed b, Cenozoic Plants and Climates of the Arctic
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  • Cenozoic Plants and Climates of the Arctic
  • Written by author Michael C. Boulter
  • Published by Springer-Verlag New York, LLC, 11/22/2011
  • Fifty million years ago, the Arctic Ocean was a warm sea, bounded by lush vegetation of the warm-temperate shores of Scandinavia, Siberia, Alaska and the Northwest Territories. Wind and storms were rare because Atlantic weather systems had not developed b
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Preface
Towards a Review of Tertiary Palaeobotany in the Boreal Realm 1
Fossil Plants as Palaeoenvironmental Indicators 13
Palaeo-Ecophysiological Studies on Cretaceous and Tertiary Fossil Floras 23
Cenozoic Tectono-Magmatic Events in the North Atlantic: Potential Palaeo-Environmental Implications 35
Cenozoic Dinoflagellate Palaeoecology Elucidated, and Used for Marine-Terrestrial Biological Correlation 57
Late Eocene-Oligocene Dinoflagellate Provincialism in the North Atlantic Ocean 73
Dinoflagellate Cysts and Climate Change Through the Neogene 93
Comparison of Palaeo Data Based on Plant and Foraminiferal Evidence from the Cenozoic of Northeast Asia (Koryak Hills, Kamchatka) 107
Tertiary Climate Changes in the Far East Based on Palaeofloristic and Palaeomagnetic Data 115
A Review of Late Cretaceous Floras and Climates of Arctic Russia 127
Late Cretaceous Artic Platanoids and High Latitude Climate 151
Circum-Arctic Plant Fossils and the Cretaceous-Tertiary Transition 161
Early Tertiary Vegetation of Arctic Canada and Its Relevance to Paleoclimatic Interpretation 175
Two Conifers - Tetraclinis Mast. (Cupressaceae) and Metasequoia Miki (Taxodiaceae) - Relicts or Palaeoclimatic Indicators of the Past 199
The Palaeogene Flora of Spitsbergen: Implications for Arcto-Tertiary Climatostratigraphy 215
Alaskan Palaeogene Climates as Inferred from the Clamp Database 223
Invasion of Arcto-Tertiary Elements in the Paleogene of Central Europe 239
Connecting Links Between the Arctic Paleocene and European Tertiary Floras 251
An Estimate of the Early Tertiary Paleoclimate of the Southern Arctic 267
The Fossil of the Paleogene Climatic Optimum in North Eastern Asia 297
Some Early Paleocene Species from western Kamchatka 315
Migrations and Evolution: Computerised Maps from Computerised Data 327
Floristic Changes in the Areas Surrounding the Paratethys During Neogene Time 347
Some Late Pliocene and Early Pleistocene Pollen Profiles from Poland 371
Arcto-Tertiary '93: Perspectives and Prospects 383
Plans for Further International Cooperation 389
Subject Index 399


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Cenozoic Plants and Climates of the Arctic, Fifty million years ago, the Arctic Ocean was a warm sea, bounded by lush vegetation of the warm-temperate shores of Scandinavia, Siberia, Alaska and the Northwest Territories. Wind and storms were rare because Atlantic weather systems had not developed b, Cenozoic Plants and Climates of the Arctic

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Cenozoic Plants and Climates of the Arctic, Fifty million years ago, the Arctic Ocean was a warm sea, bounded by lush vegetation of the warm-temperate shores of Scandinavia, Siberia, Alaska and the Northwest Territories. Wind and storms were rare because Atlantic weather systems had not developed b, Cenozoic Plants and Climates of the Arctic

Cenozoic Plants and Climates of the Arctic

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Cenozoic Plants and Climates of the Arctic, Fifty million years ago, the Arctic Ocean was a warm sea, bounded by lush vegetation of the warm-temperate shores of Scandinavia, Siberia, Alaska and the Northwest Territories. Wind and storms were rare because Atlantic weather systems had not developed b, Cenozoic Plants and Climates of the Arctic

Cenozoic Plants and Climates of the Arctic

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