Titlebook: Late Cainozoic Floras of Iceland; 15 Million Years of Thomas Denk,Friðgeir Grimsson,Leifur A. Símonarson Book 2011 Springer Science+Busine

pessimism

MEAN

ascend

GROSS

RALES

Stagger

,The Early Late Miocene Floras – First Evidence of Cool Temperate and Herbaceous Taxa,new elements are . and the extinct Fagaceae ., both of which are documented by their pollen. . and . are other taxa that appear for the first time in Iceland. In this chapter, the taxonomic composition of the 10 Ma floras of Iceland has been investigated. In addition, floristic turnovers between 12

RUPT

,The Middle Late Miocene Floras – A Window into the Regional Vegetation Surrounding a Large Caldera,determined the presence of . or . as is also seen today in cool temperate regions of the northern hemisphere. Overall, the climate appears to be more diversified than in the older floras with relatively warmer humid conditions windward of the mountains or in sheltered areas close to the lake and coo

倒转

A Late Messinian Palynoflora with a Distinct Taphonomy,es of Ericaceae). The occurrence of a new type of . with clear biogeographic affinities to North America points to a functioning land bridge between Iceland and Greenland during the Late Miocene and to climatic conditions in northern North America and Greenland that would have allowed for migration

最高点

,Pliocene Terrestrial and Marine Biota of the Tjörnes Peninsula: Warm Climates and Biogeographic Re-ates into the North Atlantic. Plant fossils recovered from the Tjörnes beds originate from three localities. Sediments exposed at the Egilsgjóta (4.3–4.2 Ma) and Reká (4.2–4.0 Ma) localities are part of the . Zone while those from Skeifá (3.9–3.8) belong to the . Zone. The fossil flora does not show

Indent