2961777676d8db46c072f38e92d68922 diversity_a2023v15n3p390.pdf 295c2b049b8d911bbb156f5246d5791e7989d481 diversity_a2023v15n3p390.pdf 9fa488877f47f7e9e7fe36a18bdcf39340ada4273be838fbbc691ceb5c10a3cd diversity_a2023v15n3p390.pdf Title: Paleoenvironmental Reconstruction for the Last 3500 Years in the Southern Pyrenees from a Peat Bog Core in Clots de Rialba Subject: Vegetation landscape dynamics are derived from the relationships established between anthropic activities and climate conditions over time. Paleoenvironmental research in the Pyrenees range (north-eastern Iberian Peninsula) has revealed what these dynamics were like in some regions during the Holocene. However, some fields of biogeography still present questions that need to be addressed, such as the patterns of Fagus sylvatica and Abies alba and the importance of the fire regime during the Meghalayan (late Holocene). We present a multiproxy study performed in a sedimentary record from the Clots de Rialba peat bog, located at 2093 m a. s. l. (Lleida, southern slope of the Pyrenees mountain range), that covers the last c. 3500 years. Analyses were performed on the organic matter content, pollen, non-pollen palynomorphs, and sedimentary charcoals larger than 150 m. The palynological spectra revealed a maximum extension of Abies alba at about 3500 cal yr BP in the Bronze Age, while Fagus sylvatica showed its maximum extent between 3300 and 2800 cal yr BP. A dominance of Pinus was detected throughout the studied period. Other taxa such as cereals, herbaceous plants, aquatic plants, and coprophilous fungi have also been discussed to identify anthropic pressure and climate pulses. In addition, the study of sedimentary charcoals reveals the main forest fire episodes and their recurrences, some of them linked to anthropogenic activities and/or climate variations. These anthropogenic activities would include the use of opening and maintaining forest fires in deforestation in order to obtain pastures and spaces dedicated to cereal agriculture and the appearance of some taxa linked to or introduced by human communities. Keywords: Meghalayan; Abies alba; Fagus sylvatica; Pyrenees; sedimentary charcoals; forest fires Author: Josep-Manel Rodríguez-González, Marc Sánchez-Morales, Jordi Nadal-Tersa, Albert Pèlachs and Ramon Pérez-Obiol Creator: LaTeX with hyperref Producer: pdfTeX-1.40.21 CreationDate: Mon Mar 13 09:17:10 2023 CET ModDate: Mon Mar 13 09:27:39 2023 CET Tagged: no UserProperties: no Suspects: no Form: none JavaScript: no Pages: 17 Encrypted: no Page size: 595.276 x 841.89 pts (A4) Page rot: 0 File size: 4332093 bytes Optimized: no PDF version: 1.7 name type encoding emb sub uni object ID ------------------------------------ ----------------- ---------------- --- --- --- --------- AWCVSS+VnURWPalladioL Type 1 Custom yes yes no 10 0 OVNEXW+EURM10 Type 1 Builtin yes yes no 15 0 PHYQAM+URWPalladioL-Bold Type 1 Custom yes yes no 19 0 YZRPPX+URWPalladioL-Roma Type 1 Custom yes yes no 24 0 QYAIGX+URWPalladioL-Ital Type 1 Custom yes yes no 28 0 DPDBQY+VnURWPalladioL-Bold Type 1 Custom yes yes no 32 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RepresentationInformation: diversity_a2023v15n3p390.pdf ReportingModule: PDF-hul, Rel. 1.12.4 (2023-03-16) LastModified: 2024-01-31 20:42:33 CET Size: 4332093 Format: PDF Version: 1.7 Status: Well-Formed and valid SignatureMatches: PDF-hul MIMEtype: application/pdf PDFMetadata: Objects: 563 FreeObjects: 1 IncrementalUpdates: 0 DocumentCatalog: PageLayout: SinglePage PageMode: UseNone Outlines: Item: Title: Introduction Destination: section.1 Item: Title: Study Area Destination: section.2 Item: Title: Materials and Methods Destination: section.3 Children: Item: Title: Samples Destination: subsection.3.1 Item: Title: Chronology Destination: subsection.3.2 Item: Title: Organic Material Destination: subsection.3.3 Item: Title: Palynology Destination: subsection.3.4 Item: Title: Sedimentary Charcoals Destination: subsection.3.5 Item: Title: Results Destination: section.4 Children: Item: Title: Sedimentary Description and Organic Matter Destination: subsection.4.1 Item: Title: Pollen and Sedimentary Charcoals (>150 m) Destination: subsection.4.2 Children: Item: Title: CdR1-APAZ. from c. 3500 to 2850 cal yr BP Destination: subsubsection.4.2.1 Item: Title: CdR1-BPAZ. from c. 2850 to 2500 cal yr BP Destination: subsubsection.4.2.2 Item: Title: CdR1-CPAZ. from c. 2500 to 800 cal yr BP Destination: subsubsection.4.2.3 Item: Title: CdR1-DPAZ. from c. 800 to 450 cal yr BP Destination: subsubsection.4.2.4 Item: Title: CdR1-EPAZ. from c. 450 cal yr BP to the Present Day Destination: subsubsection.4.2.5 Item: Title: Discussion Destination: section.5 Children: Item: Title: Landscape Evolution from the Bronze Age to the Iron Age (from c. 3500 to 2200 cal yr BP) Destination: subsection.5.1 Item: Title: Landscape Evolution during the Roman Period (from c. 2200 to 1500 cal yr BP) Destination: subsection.5.2 Item: Title: Landscape Evolution during the Medieval Ages and the Little Ice Age (from c. 1500 cal yr BP to the Present) Destination: subsection.5.3 Item: Title: Conclusions Destination: section.6 Item: Title: References Destination: section.6 Info: Title: Paleoenvironmental Reconstruction for the Last 3500 Years in the Southern Pyrenees from a Peat Bog Core in Clots de Rialba Author: Josep-Manel Rodríguez-González, Marc Sánchez-Morales, Jordi Nadal-Tersa, Albert Pèlachs and Ramon Pérez-Obiol Subject: Vegetation landscape dynamics are derived from the relationships established between anthropic activities and climate conditions over time. Paleoenvironmental research in the Pyrenees range (north-eastern Iberian Peninsula) has revealed what these dynamics were like in some regions during the Holocene. However, some fields of biogeography still present questions that need to be addressed, such as the patterns of Fagus sylvatica and Abies alba and the importance of the fire regime during the Meghalayan (late Holocene). We present a multiproxy study performed in a sedimentary record from the Clots de Rialba peat bog, located at 2093 m a. s. l. (Lleida, southern slope of the Pyrenees mountain range), that covers the last c. 3500 years. Analyses were performed on the organic matter content, pollen, non-pollen palynomorphs, and sedimentary charcoals larger than 150 m. The palynological spectra revealed a maximum extension of Abies alba at about 3500 cal yr BP in the Bronze Age, while Fagus sylvatica showed its maximum extent between 3300 and 2800 cal yr BP. A dominance of Pinus was detected throughout the studied period. Other taxa such as cereals, herbaceous plants, aquatic plants, and coprophilous fungi have also been discussed to identify anthropic pressure and climate pulses. In addition, the study of sedimentary charcoals reveals the main forest fire episodes and their recurrences, some of them linked to anthropogenic activities and/or climate variations. These anthropogenic activities would include the use of opening and maintaining forest fires in deforestation in order to obtain pastures and spaces dedicated to cereal agriculture and the appearance of some taxa linked to or introduced by human communities. 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