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https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/#enrichment_service-account-enrichment http://schema.org/name service-account-enrichment https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/#enrichment_service-account-enrichment http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://xmlns.com/foaf/0.1/Agent https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/about http://eurovoc.europa.eu/1151 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/about http://eurovoc.europa.eu/5028 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/author https://orcid.org/0000-0002-2736-0052 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/contentSize 6189 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/contentUrl https://api.rohub.org/api/ros/f0b9d343-156c-46e2-aa72-efb121a12265/crate/download/ https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/creator mailto:service-account-generation-service https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/dateCreated 2021-12-10 10:07:07.030356+00:00 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/dateModified 2025-03-05 12:47:15.829950+00:00 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/datePublished 2021-12-10 10:07:07.030356+00:00 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/description The southern Alpine foreland, facing windward to moist southern airmasses, is daimed to have supported forest vegetation throughout the Last Glaciation. Here we present a multiproxy paleoecological record from a compressed peat, uncovered at Casaletto Ceredano, N-Italy, spanning the interval from 33 to 30.5 kyr cal BP. Stratigraphically, it underlies a fluvioglacial belt attributed to the Last Glacial Maximum.The peat records a floodplain swamp community with tree birch and tall sedges, pine woodlands in upland areas, and only limited patches of open vegetation. Plant macrofossils - bark, charcoal, wood and fruits - establish the predominant role of Betulu pubescens group (downy birch) in the anoxic wetland, thanks to its ability to enhance gas exchange through a distinctive type of bark lenticels. A fire-induced birch-to-pine cyde is repeated twice along the 2500 years-time span covered by the peat layer. The climate reconstructed from modern pollen analogs compares to northern boreal zone, with Tjuly <15 degrees C, excluding warm-temperate trees. A major flood sealing the swamp with minerogenic silt is precisely dated to 30,497 +/- 594 yr cal BP (2 sigma uncertainty). Here, the pollen record shows a substantial forest withdrawal, and development of grasslands and semideserts, pointing to co-factorial action of increased climate continentality and of river dynamics. According to teleconnections with the Atlantic and Arctic framework of the stadial-interstadial climate variability, the age and pattern of this event are consistent with the onset of Heinrich Stadial 3, causing a lockdown of moist westerlies and of their Rossby waves in the W-Mediterranean. (C) 2020 Elsevier B.V. All rights reserved. https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/encodingFormat application/ld+json https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/hasPart https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/resources/7ba72c0c-694e-464a-b488-342c736d7c0e https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/identifier https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/license https://choosealicense.com/no-permission/ https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://schema.org/name Birch-sedge communities, forest withdrawal and flooding at the beginning of Heinrich Stadial 3 at the southern Alpine foreland https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://w3id.org/ro-id/rohub/model#creation_mode MANUAL https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/ro#ResearchObject https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://purl.org/wf4ever/roevo#LiveRO https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://schema.org/Dataset https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type http://w3id.org/ro/earth-science#BibliographyResearchObject https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ http://www.w3.org/1999/02/22-rdf-syntax-ns#type https://w3id.org/ro/terms/earth-science#BibliographyResearchObject https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/ https://www.w3.org/ns/iana/link-relations/relation#cite-as Foglini, Federica. "Birch-sedge communities, forest withdrawal and flooding at the beginning of Heinrich Stadial 3 at the southern Alpine foreland." ROHub. Dec 10 ,2021. https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265. https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/resources/7ba72c0c-694e-464a-b488-342c736d7c0e http://schema.org/author mailto:service-account-generation-service https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/resources/7ba72c0c-694e-464a-b488-342c736d7c0e http://schema.org/contentSize 284 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/resources/7ba72c0c-694e-464a-b488-342c736d7c0e http://schema.org/contentUrl https://api.rohub.org/api/resources/7ba72c0c-694e-464a-b488-342c736d7c0e/download/ https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/resources/7ba72c0c-694e-464a-b488-342c736d7c0e http://schema.org/creator mailto:service-account-generation-service https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/resources/7ba72c0c-694e-464a-b488-342c736d7c0e http://schema.org/dateCreated 2021-12-10 10:07:09.858283+00:00 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/resources/7ba72c0c-694e-464a-b488-342c736d7c0e http://schema.org/dateModified 2021-12-10 10:07:09.859316+00:00 https://w3id.org/ro-id/f0b9d343-156c-46e2-aa72-efb121a12265/resources/7ba72c0c-694e-464a-b488-342c736d7c0e http://schema.org/description The southern Alpine foreland, facing windward to moist southern airmasses, is daimed to have supported forest vegetation throughout the Last Glaciation. Here we present a multiproxy paleoecological record from a compressed peat, uncovered at Casaletto Ceredano, N-Italy, spanning the interval from 33 to 30.5 kyr cal BP. Stratigraphically, it underlies a fluvioglacial belt attributed to the Last Glacial Maximum.The peat records a floodplain swamp community with tree birch and tall sedges, pine woodlands in upland areas, and only limited patches of open vegetation. Plant macrofossils - bark, charcoal, wood and fruits - establish the predominant role of Betulu pubescens group (downy birch) in the anoxic wetland, thanks to its ability to enhance gas exchange through a distinctive type of bark lenticels. A fire-induced birch-to-pine cyde is repeated twice along the 2500 years-time span covered by the peat layer. The climate reconstructed from modern pollen analogs compares to northern boreal zone, with Tjuly <15 degrees C, excluding warm-temperate trees. A major flood sealing the swamp with minerogenic silt is precisely dated to 30,497 +/- 594 yr cal BP (2 sigma uncertainty). Here, the pollen record shows a substantial forest withdrawal, and development of grasslands and semideserts, pointing to co-factorial action of increased climate continentality and of river dynamics. According to teleconnections with the Atlantic and Arctic framework of the stadial-interstadial climate variability, the age and pattern of this event are consistent with the onset of Heinrich Stadial 3, causing a lockdown of moist westerlies and of their Rossby waves in the W-Mediterranean. (C) 2020 Elsevier B.V. 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