date: 2022-02-21T07:48:33Z pdf:unmappedUnicodeCharsPerPage: 17 pdf:PDFVersion: 1.7 pdf:docinfo:title: Holocene Hydroclimatic Changes in Northern Peloponnese (Greece) Inferred from the Multiproxy Record of Lake Lousoi xmp:CreatorTool: LaTeX with hyperref Keywords: XRF; polje; paleoenvironment; paleoclimate; eastern Mediterranean access_permission:modify_annotations: true access_permission:can_print_degraded: true subject: This research presents the paleoenvironmental evolution of a drained lake at the Lousoi plateau (northern Peloponnese), for the last 10,000 years, through the study of a 7 m depth core. Analyses conducted on the core include grain size, TOC, TN, pH, EC, total carbonates (%), magnetic susceptibility measurements, XRF analysis, and radiocarbon dating. Our paleoenvironmental reconstruction was based on geochemical proxies? distribution in the core, combined with sediment physical and textural characteristics and later comparison between additional lacustrine archives from northern Peloponnese. From 10,900 to 7700 cal BP lacustrine, organic-rich deposits were recognized, reflecting increased lake water levels. Wet climatic conditions seem to have prevailed during this phase, interrupted by a dry pulse at 9400 cal BP. Transition to more shallow waters was marked at 8200 cal BP due to increased sediment deposition in the lake, with the environmental status shifting to a more oxygenated phase. Overall, wet conditions prevailed in this period and are in good agreement with regional records. In the Late Holocene period, the lake seems to have been highly affected by pedogenic processes, and thus, it was difficult to distinguish paleoclimatic/paleoenvironmental signals. dc:creator: Dionysios Stamatis, Alexandros Emmanouilidis, Alessia Masi, Adam Izdebski and Pavlos Avramidis dcterms:created: 2022-02-21T07:25:19Z Last-Modified: 2022-02-21T07:48:33Z dcterms:modified: 2022-02-21T07:48:33Z dc:format: application/pdf; version=1.7 title: Holocene Hydroclimatic Changes in Northern Peloponnese (Greece) Inferred from the Multiproxy Record of Lake Lousoi Last-Save-Date: 2022-02-21T07:48:33Z pdf:docinfo:creator_tool: LaTeX with hyperref access_permission:fill_in_form: true pdf:docinfo:keywords: XRF; polje; paleoenvironment; paleoclimate; eastern Mediterranean pdf:docinfo:modified: 2022-02-21T07:48:33Z meta:save-date: 2022-02-21T07:48:33Z pdf:encrypted: false dc:title: Holocene Hydroclimatic Changes in Northern Peloponnese (Greece) Inferred from the Multiproxy Record of Lake Lousoi modified: 2022-02-21T07:48:33Z cp:subject: This research presents the paleoenvironmental evolution of a drained lake at the Lousoi plateau (northern Peloponnese), for the last 10,000 years, through the study of a 7 m depth core. Analyses conducted on the core include grain size, TOC, TN, pH, EC, total carbonates (%), magnetic susceptibility measurements, XRF analysis, and radiocarbon dating. Our paleoenvironmental reconstruction was based on geochemical proxies? distribution in the core, combined with sediment physical and textural characteristics and later comparison between additional lacustrine archives from northern Peloponnese. From 10,900 to 7700 cal BP lacustrine, organic-rich deposits were recognized, reflecting increased lake water levels. Wet climatic conditions seem to have prevailed during this phase, interrupted by a dry pulse at 9400 cal BP. Transition to more shallow waters was marked at 8200 cal BP due to increased sediment deposition in the lake, with the environmental status shifting to a more oxygenated phase. Overall, wet conditions prevailed in this period and are in good agreement with regional records. In the Late Holocene period, the lake seems to have been highly affected by pedogenic processes, and thus, it was difficult to distinguish paleoclimatic/paleoenvironmental signals. pdf:docinfo:subject: This research presents the paleoenvironmental evolution of a drained lake at the Lousoi plateau (northern Peloponnese), for the last 10,000 years, through the study of a 7 m depth core. Analyses conducted on the core include grain size, TOC, TN, pH, EC, total carbonates (%), magnetic susceptibility measurements, XRF analysis, and radiocarbon dating. Our paleoenvironmental reconstruction was based on geochemical proxies? distribution in the core, combined with sediment physical and textural characteristics and later comparison between additional lacustrine archives from northern Peloponnese. From 10,900 to 7700 cal BP lacustrine, organic-rich deposits were recognized, reflecting increased lake water levels. Wet climatic conditions seem to have prevailed during this phase, interrupted by a dry pulse at 9400 cal BP. Transition to more shallow waters was marked at 8200 cal BP due to increased sediment deposition in the lake, with the environmental status shifting to a more oxygenated phase. Overall, wet conditions prevailed in this period and are in good agreement with regional records. In the Late Holocene period, the lake seems to have been highly affected by pedogenic processes, and thus, it was difficult to distinguish paleoclimatic/paleoenvironmental signals. Content-Type: application/pdf pdf:docinfo:creator: Dionysios Stamatis, Alexandros Emmanouilidis, Alessia Masi, Adam Izdebski and Pavlos Avramidis X-Parsed-By: org.apache.tika.parser.DefaultParser creator: Dionysios Stamatis, Alexandros Emmanouilidis, Alessia Masi, Adam Izdebski and Pavlos Avramidis meta:author: Dionysios Stamatis, Alexandros Emmanouilidis, Alessia Masi, Adam Izdebski and Pavlos Avramidis dc:subject: XRF; polje; paleoenvironment; paleoclimate; eastern Mediterranean meta:creation-date: 2022-02-21T07:25:19Z created: 2022-02-21T07:25:19Z access_permission:extract_for_accessibility: true access_permission:assemble_document: true xmpTPg:NPages: 12 Creation-Date: 2022-02-21T07:25:19Z pdf:charsPerPage: 3910 access_permission:extract_content: true access_permission:can_print: true meta:keyword: XRF; polje; paleoenvironment; paleoclimate; eastern Mediterranean Author: Dionysios Stamatis, Alexandros Emmanouilidis, Alessia Masi, Adam Izdebski and Pavlos Avramidis producer: pdfTeX-1.40.21 access_permission:can_modify: true pdf:docinfo:producer: pdfTeX-1.40.21 pdf:docinfo:created: 2022-02-21T07:25:19Z