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• W2140993687 abstract "Abstract The inception of terrestrial woody plant ecosystems on the Earth is thought to have caused decreases in atmospheric carbon dioxide and water vapor concentrations in the Middle Devonian. Decreased greenhouse gas concentrations enabled a series of long-term glacial-interglacial cycles from the Late Devonian through the Permian. Here we describe the environmental and ecological variability of the earliest known paleosols with evidence of in situ forests (stump casts and attached root systems) from the Appalachian basin. Four examples located in the Manorkill Formation in the Catskill Mountains of New York State, United States, are analyzed using macro- and micromorphological data. Woody plant stump casts and molds on exposed bedding surfaces were mapped at two of the sites and analyzed using nearest-neighbor analysis. This permitted quantification of spatial distribution and ecological conditions of these paleoforests. These fossilized forests exhibit both single and multi-generational growth and fo..." @default.
• W2140993687 created "2016-06-24" @default.
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• W2140993687 date "2010-01-22" @default.
• W2140993687 modified "2023-09-25" @default.
• W2140993687 title "ENVIRONMENTAL AND ECOLOGICAL VARIABILITY OF MIDDLE DEVONIAN (GIVETIAN) FORESTS IN APPALACHIAN BASIN PALEOSOLS, NEW YORK, UNITED STATES" @default.
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• W2140993687 doi "https://doi.org/10.2110/palo.2009.p09-086r" @default.
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