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Titlebook: Nature through Time; Virtual field trips Edoardo Martinetto,Emanuel Tschopp,Robert A. Gasta Textbook 2020 Springer Nature Switzerland AG 2

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,The Paleocene–Eocene Thermal Maximum: Plants as Paleothermometers, Rain Gauges, and Monitors,rica before, during, and right after this thermal maximum. Lastly, we explore how fossil data can be incorporated with ecological and systematic information into biogeographical models to predict how plants respond to climate change.
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Long-Lasting Morphologies Despite Evolution: Ferns (Monilophytes) Throughout the Phanerozoic,ide of pinnules. Although growth forms show great variability in morphology and size, all have retained this simple reproductive organization for over 400 million years from when first recognized in Devonian floras.
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2510-1307 osystems in the Mesozoic, the Permian mass extinction, the late Paleozoic glaciation, and the origin of the first trees and land plants in the Devonian-Ordovician. With state-of-the art expert scientific instru978-3-030-35060-4978-3-030-35058-1Series ISSN 2510-1307 Series E-ISSN 2510-1315
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Triumph and Fall of the Wet, Warm, and Never-More-Diverse Temperate Forests (Oligocene-Pliocene), lineages adapted to cooler conditions and entered the warmer temperate realm. An equable climate with abundant precipitation in widespread areas provided a suitable habitat for moisture-requiring woody plants. The higher floristic diversity in the Neogene compared to the present is best illustrated
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Aridity, Cooling, Open Vegetation, and the Evolution of Plants and Animals During the Cenozoic,ores, favoring forms with hypsodont teeth. In Europe, where humid climates generally persisted throughout the Neogene, the Iberian Peninsula was the first region to experience increasingly seasonal aridity in the early Miocene. Open environments under an arid climate remained confined to Southern Eu
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