Item talk:Q240381
From geokb
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"abstract": "The timing and drivers of vegetation dynamics and formation of no-analog plant communities during the last deglaciation in the unglaciated southeastern US are poorly understood. We present a multi-proxy record spanning the past 19,800 years from Cupola Pond in the Ozarks Mountains, consisting of replicate high-resolution pollen records, 25 AMS radiocarbon dates, and macrofossil, charcoal, and coprophilous spore analyses. Full-glacial\u00a0Pinus\u00a0and\u00a0Picea\u00a0forests gave way to no-analog vegetation after 17,400\u00a0yr BP, followed by development of\u00a0Quercus-dominated Holocene forests, with late Holocene rises in\u00a0Pinus\u00a0and\u00a0Nyssa. Vegetation transitions, replicated in different cores, are closely linked to hemispheric climate events. Rising\u00a0Quercus\u00a0abundances coincide with increasing Northern Hemisphere temperatures and CO2\u00a0at 17,500\u00a0yr BP, declining\u00a0Pinus\u00a0and\u00a0Picea\u00a0at 14,500\u00a0yr BP are near the B\u00f8lling-Aller\u00f8d onset, and rapid decline of\u00a0Fraxinus\u00a0and rise of\u00a0Ostrya/Carpinus\u00a0occur 12,700\u00a0yr BP during the Younger Dryas. The Cupola no-analog vegetation record is unusual for its early initiation (17,000\u00a0yr BP) and for its three vegetation zones, representing distinct rises of\u00a0Fraxinus\u00a0and\u00a0Ostrya/Carpinus.\u00a0Sporormiella\u00a0was absent and sedimentary charcoal abundances were low throughout, suggesting that fire and megaherbivores were not locally important agents of disturbance and turnover. The Cupola record thus highlights the complexity of the late-glacial no-analog communities and suggests direct climatic regulation of their formation and disassembly.",
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