Fiona Cornet, Vincent Montade, Stéphanie C. Bodin, Justine Descloitre, Maxime Réjou-Méchain, Gaëlle Viennois, Julie C. Aleman, Chimène Assi-Kaudjhis, William F. Kenney, Richard Oslisly, Monique G. Tossou, Laurent Bremond, Charly Favier
{"title":"From shape to source: sedimentary charcoal morphology as a proxy for tropical burned biomass composition","authors":"Fiona Cornet, Vincent Montade, Stéphanie C. Bodin, Justine Descloitre, Maxime Réjou-Méchain, Gaëlle Viennois, Julie C. Aleman, Chimène Assi-Kaudjhis, William F. Kenney, Richard Oslisly, Monique G. Tossou, Laurent Bremond, Charly Favier","doi":"10.1002/jqs.70053","DOIUrl":"https://doi.org/10.1002/jqs.70053","url":null,"abstract":"<p>Sedimentary charcoal elongation is increasingly being used in paleoecology to distinguish herbaceous from woody fuel in past fires. However, the relationship between charcoal morphotypes and plant types has never been formally tested in tropical environments, despite its potential to improve understanding of fire regimes and deforestation, and to analyze long-term ecosystem resilience. Separation between herbaceous and woody charcoal commonly relies on a fixed elongation threshold, but this arbitrary division overlooks the morphological continuum of charcoal and may bias interpretations. To address this, we developed a Bayesian model to classify charcoal fragments into herbaceous and woody subpopulations based on their elongation distributions. We applied it to 19 sediment charcoal records spanning the last 30 years across a broad geographic and vegetation gradient in West and Central Africa. Compared with contemporary vegetation cover derived from remote sensing, the estimated proportion of woody charcoal was significantly positively correlated with tree cover, validating our approach and confirming charcoal elongation as a reliable proxy for past fire-related biomass sources. Finally, we applied the model to a paleosequence from Lake Sélé (Benin) to reconstruct temporal changes in biomass and compared results with fossil pollen data, further assessing the proxy relevance for reconstructing past fire regimes and advancing tropical paleoecology.</p>","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"41 3","pages":"490-506"},"PeriodicalIF":2.2,"publicationDate":"2026-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/jqs.70053","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147686239","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Russell W. Graham, Robert E. Warren, Edwin R. Hajic, Terrence J. Frest, Donald P. Schwert, Jacqueline A. Ferguson, Melissa I. Pardi, Eric C. Grimm, Frances B. King
{"title":"Paleoenvironments of the Late Quaternary Tonica thermokarst lake, northeastern Illinois, USA, and an extinct elk-moose (Cervalces)","authors":"Russell W. Graham, Robert E. Warren, Edwin R. Hajic, Terrence J. Frest, Donald P. Schwert, Jacqueline A. Ferguson, Melissa I. Pardi, Eric C. Grimm, Frances B. King","doi":"10.1002/jqs.70045","DOIUrl":"https://doi.org/10.1002/jqs.70045","url":null,"abstract":"<div>\u0000 \u0000 <p>The Tonica Depression (TD), a late Quaternary sediment-filled basin in northeastern Illinois, formed as a thermokarst lake as evidenced by a basal trash layer, its depositional history, and its occurrence on a late-Pleistocene permafrost landscape. Stratigraphy and radiocarbon ages reveal that a multiproxy paleoenvironmental record extends throughout the late Wisconsin. Burning of organically enriched sediments has abbreviated the Holocene sequence. The lowest stratum is a glacial diamicton that forms the basin's floor, and at a slightly higher elevation, the rim. Lithofacies 1, supraglacial and debris flow deposits, are draped by undated Peoria Silt (PS). PS yielded molluscs and Coleoptera indicative of spruce forest (<i>Picea</i>) in a cold and harsh climate. Lithofacies 2 (ca. 17 500–18 500 cal yr BP) is a “trash zone” with white spruce (<i>Picea glauca</i>) wood, cones and needles with pollen, Coleoptera, molluscs, and vertebrates, including an elk-moose. A “marl,” Lithofacies 3 (ca. 14 600–17 400 cal yr BP), attests to the deepening of the lake (>2 m) as also reflected by the molluscs, coleoptera, and pollen. The environment was an open spruce forest, but the climate was warmer than the previous ones. The top of this zone is composed of a brick-red deposit with burned organic matter. Lithofacies 4 (ca. 14 600 cal yr BP) is composed of organic silt and lacustrine organic silt: a peaty silt loam. Finally, Middle Archaic artifacts on the rim of TD document human settlement around the depression during the dry and warm Middle Holocene (ca. 6747 cal BP). Tonica is the first well-studied thermokarst lake from temperate latitudes in the United States, and it provides an excellent paleoenvironmental record of the late Pleistocene of north central Illinois.</p></div>","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"41 3","pages":"433-451"},"PeriodicalIF":2.2,"publicationDate":"2026-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147686053","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Dayang Siti Maryam Binti Mohd Hanan, Katherine Selby, Sarah L Bradley, Sally Derrett
{"title":"Holocene palaeoenvironmental reconstruction of sea level, coastal and vegetation changes along the southern Solway Firth, United Kingdom","authors":"Dayang Siti Maryam Binti Mohd Hanan, Katherine Selby, Sarah L Bradley, Sally Derrett","doi":"10.1002/jqs.70052","DOIUrl":"https://doi.org/10.1002/jqs.70052","url":null,"abstract":"<p>Holocene relative sea level (RSL) changes were reconstructed from four sites along the less-studied southern Solway Firth. A multiproxy approach, including lithostratigraphical and biostratigraphical analyses, combined with radiocarbon dating, produced ten sea level index points (SLIPs). These SLIPs constrained Holocene RSL changes in the region between ~8300 cal BP and ~6018 cal BP and captured the Main Postglacial Transgression. These ten new points are combined with the ten pre-existing SLIPS from the southern Solway Firth to greatly refine the trend of Holocene RSL changes across this region. The Main Postglacial Transgression was shown to occur between ~8320 and 7500 cal BP, reaching a highstand of 3.26 ± 0.56 mOD. The new data were combined with 73 existing SLIPS from two sites around the northern Solway Firth and compared to RSL predictions from glacial isostatic modelling. Comparison between the corrected SLIPs and RSL predictions using British and Irish ice sheet reconstructions showed that the timing of the Main Postglacial Transgression is best captured with a hybrid model for the presence of thick and thin ice sheets. Pollen analysis at Cowgate Farm and Herd Hill provided a record of vegetation and coastal changes, acting as a chronostratigraphic marker when compared to published pollen records of the region. The records show a general transition from saltmarsh to reed swamp, then peat bog as RSL declined through the mid to late Holocene, with some indications of human clearance in the Bronze Age.</p>","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"41 3","pages":"419-432"},"PeriodicalIF":2.2,"publicationDate":"2026-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/jqs.70052","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147686087","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Micromorphology: A practical guide to the microscale analysis of glacial sediments and processes Edited by \u0000 Emrys Phillips and \u0000 John Menzies, 2025, Published by the Quaternary Research Association, ISBN: 0 907780 296 242; ISSN: 0264 9241","authors":"Lewis A. Owen","doi":"10.1002/jqs.70055","DOIUrl":"https://doi.org/10.1002/jqs.70055","url":null,"abstract":"","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"41 3","pages":"540-541"},"PeriodicalIF":2.2,"publicationDate":"2026-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147686238","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}