Journal of Quaternary Science最新文献

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From shape to source: sedimentary charcoal morphology as a proxy for tropical burned biomass composition 从形状到来源:沉积木炭形态作为热带燃烧生物量组成的代表
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-02-24 DOI: 10.1002/jqs.70053
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,&nbsp;Vincent Montade,&nbsp;Stéphanie C. Bodin,&nbsp;Justine Descloitre,&nbsp;Maxime Réjou-Méchain,&nbsp;Gaëlle Viennois,&nbsp;Julie C. Aleman,&nbsp;Chimène Assi-Kaudjhis,&nbsp;William F. Kenney,&nbsp;Richard Oslisly,&nbsp;Monique G. Tossou,&nbsp;Laurent Bremond,&nbsp;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}
引用次数: 0
Paleoenvironments of the Late Quaternary Tonica thermokarst lake, northeastern Illinois, USA, and an extinct elk-moose (Cervalces) 美国伊利诺斯州东北部晚第四纪Tonica热岩溶湖的古环境与一种已灭绝的麋鹿(Cervalces)
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-02-16 DOI: 10.1002/jqs.70045
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,&nbsp;Robert E. Warren,&nbsp;Edwin R. Hajic,&nbsp;Terrence J. Frest,&nbsp;Donald P. Schwert,&nbsp;Jacqueline A. Ferguson,&nbsp;Melissa I. Pardi,&nbsp;Eric C. Grimm,&nbsp;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 (&gt;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}
引用次数: 0
Holocene palaeoenvironmental reconstruction of sea level, coastal and vegetation changes along the southern Solway Firth, United Kingdom 英国索尔威湾南部海平面、海岸和植被变化的全新世古环境重建
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-02-11 DOI: 10.1002/jqs.70052
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,&nbsp;Katherine Selby,&nbsp;Sarah L Bradley,&nbsp;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}
引用次数: 0
Micromorphology: A practical guide to the microscale analysis of glacial sediments and processes Edited by Emrys Phillips and John Menzies, 2025, Published by the Quaternary Research Association, ISBN: 0 907780 296 242; ISSN: 0264 9241 《微观形态:冰川沉积物和过程的微尺度分析实用指南》,由Emrys Phillips和John Menzies编辑,2025年,第四纪研究协会出版,ISBN: 0 907780 296 242;发行号:0264 9241
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-02-24 DOI: 10.1002/jqs.70055
Lewis A. Owen
{"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}
引用次数: 0
From Ice to Isolation: A geochemical reconstruction of the palaeoenvironmental evolution of Gairloch, NW Scotland (UK), since the Last Glacial Maximum 从冰封到孤立:末次盛冰期以来苏格兰西北部Gairloch古环境演化的地球化学重建
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-02-26 DOI: 10.1002/jqs.70057
Jennifer Taylor, David Selby, Jeremy M. Lloyd, Louise Best, Luca Podrecca, Bradley B. Sageman, Alexander R. Simms
{"title":"From Ice to Isolation: A geochemical reconstruction of the palaeoenvironmental evolution of Gairloch, NW Scotland (UK), since the Last Glacial Maximum","authors":"Jennifer Taylor,&nbsp;David Selby,&nbsp;Jeremy M. Lloyd,&nbsp;Louise Best,&nbsp;Luca Podrecca,&nbsp;Bradley B. Sageman,&nbsp;Alexander R. Simms","doi":"10.1002/jqs.70057","DOIUrl":"https://doi.org/10.1002/jqs.70057","url":null,"abstract":"<p>Complex relative sea-level (RSL) changes are associated with the deglaciation of the British and Irish Ice Sheet (BIIS). Sediment archives from Loch Bad na h-Achlaise, an isolation basin in NW Scotland, UK, span Late Glacial to Holocene time and record sea-level change and ice proximity via a geochemical and biostratigraphic multiproxy approach. Osmium and carbon isotope, carbon and nitrogen content, and X-ray fluorescence (XRF) data suggest that the basal sedimentary unit reflects a glaciomarine depositional setting, a finding previously unresolved due to an inadequate biostratigraphic framework. The <sup>187</sup>Os/<sup>188</sup>Os record from the basin captures the RSL history of this site and illustrates the interplay between the local signal of glacial isostatic adjustment and the non-local signal of glacio-eustatic sea-level rise. By coupling the <sup>187</sup>Os/<sup>188</sup>Os data with a detailed age–depth model, our study demonstrates a period of RSL fall between 16.2 and 15.9 cal ka BP, which culminates in basin isolation. The close agreement between the biostratigraphy, where available, and the <sup>187</sup>Os/<sup>188</sup>Os record confirms the viability of this isotope system as an RSL proxy not reliant on microfossil preservation and thus a potentially effective approach when poor microfossil preservation hampers palaeoenvironmental reconstruction.</p>","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"41 3","pages":"507-519"},"PeriodicalIF":2.2,"publicationDate":"2026-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/jqs.70057","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147686281","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}
引用次数: 0
Neanderthal incursions at a high-altitude “bear cave”: Reassessing Caverna Generosa in the southern Alps 尼安德特人在高海拔“熊洞”的入侵:重新评估南阿尔卑斯山的巨穴
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-01-13 DOI: 10.1002/jqs.70048
Davide Delpiano, Lucia Angiolini, Marco Peresani, Fabio Bona
{"title":"Neanderthal incursions at a high-altitude “bear cave”: Reassessing Caverna Generosa in the southern Alps","authors":"Davide Delpiano,&nbsp;Lucia Angiolini,&nbsp;Marco Peresani,&nbsp;Fabio Bona","doi":"10.1002/jqs.70048","DOIUrl":"https://doi.org/10.1002/jqs.70048","url":null,"abstract":"<div>\u0000 \u0000 <p>High-altitude “bear caves” provide unique windows into Middle Paleolithic human behavior, often reflecting sporadic Neanderthal occupations in challenging alpine environments. In this study, we present updated evidence from Caverna Generosa, a “bear cave” situated at 1450 m a.s.l. in the Lombard Prealps, Italy. Our research integrates new lithic analyses with recent micromorphological and paleontological data, offering a comprehensive understanding of the site's occupational history. Radiometric recalibration of existing dates, combined with comparative analyses of other high-altitude Neanderthal sites, refines the chronological framework of these occupations in a late phase of the Middle Paleolithic. Although sparse, the lithic assemblages from Caverna Generosa provide valuable insights into Neanderthal technological behaviors. The pronounced fragmentation of the reduction sequence, along with the presence of end-products, indicates a level of planning and mobility consistent with hunter–gatherer strategies in challenging environments. These results contribute to broader discussions on Neanderthal toolkits and adaptations to high-altitude habitats, highlighting the complexity of their subsistence strategies and settlement patterns. This research further underscores the importance of “bear caves” as key sites for understanding Neanderthal life in alpine regions and demonstrates the potential for integrating sporadic and episodic occupation evidence with data from more residential sites to reconstruct coherent patterns of land use and territory occupation.</p>\u0000 </div>","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"41 3","pages":"380-399"},"PeriodicalIF":2.2,"publicationDate":"2026-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147686994","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}
引用次数: 0
Origins and environmental impacts of distal rhyolitic tephra layers on Chatham Island, New Zealand 新西兰查塔姆岛远端流纹岩层的起源和环境影响
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2025-12-29 DOI: 10.1002/jqs.70046
Anna L. Miller, Simon J. Barker, Katherine A. Holt, Stephen B. Piva, Colin J. N. Wilson
{"title":"Origins and environmental impacts of distal rhyolitic tephra layers on Chatham Island, New Zealand","authors":"Anna L. Miller,&nbsp;Simon J. Barker,&nbsp;Katherine A. Holt,&nbsp;Stephen B. Piva,&nbsp;Colin J. N. Wilson","doi":"10.1002/jqs.70046","DOIUrl":"https://doi.org/10.1002/jqs.70046","url":null,"abstract":"<div>\u0000 \u0000 <p>Chatham Island, ~700 km east of mainland New Zealand, preserves several macroscopic tephra beds, sourced from the central Taupō Volcanic Zone (TVZ) some 850 km away. These layers, often enclosed within peat, provide insights into the eruptive characteristics, timing and paleoenvironmental impacts of large explosive rhyolitic eruptions in a distal setting. We report the nature, origins and impacts of these tephras by documenting bulk and centimetric-scale stratigraphic changes in glass shard geochemistry and millimetric-scale changes in pollen assemblages in the enclosing peats. Three layers are investigated: the ~25.5 ka Kawakawa–Ōruanui Tephra (KOT), the ~345 ka Rangitawa Tephra and one newly discovered tephra. The KOT shows no stratigraphic variability in glass composition throughout ~15 cm thickness. The Rangitawa Tephra contains three glass populations that were deposited sequentially throughout the eruption and further link this tephra to the Whakamaru supereruption. The new tephra has two glass populations and is matched to the ~322 ka Matahina caldera-forming eruption. High-resolution sampling of peat bracketing the KOT and Rangitawa Tephra reveals marked changes in local vegetation following the deposition of both tephras. The nature of the changes varies between events and can be explained by differing paleoenvironmental settings, climate and/or tephra thickness.</p>\u0000 </div>","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"41 3","pages":"361-379"},"PeriodicalIF":2.2,"publicationDate":"2026-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147686381","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}
引用次数: 0
Reconstructing post-crisis recovery in the hinterlands of Constantinople: A high-resolution first-millennium CE pollen record from Lake Yeniçağa (NW Türkiye) 重建君士坦丁堡腹地危机后的复苏:来自Yeniçağa湖(NW t<e:1> rkiye)的高分辨率公元一千年花粉记录
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-03-04 DOI: 10.1002/jqs.70059
Cristiano Vignola, Mustafa Doğan, Warren Eastwood, John Haldon, Alessia Masi, Neil Roberts, Çetin Şenkul, Adam Izdebski
{"title":"Reconstructing post-crisis recovery in the hinterlands of Constantinople: A high-resolution first-millennium CE pollen record from Lake Yeniçağa (NW Türkiye)","authors":"Cristiano Vignola,&nbsp;Mustafa Doğan,&nbsp;Warren Eastwood,&nbsp;John Haldon,&nbsp;Alessia Masi,&nbsp;Neil Roberts,&nbsp;Çetin Şenkul,&nbsp;Adam Izdebski","doi":"10.1002/jqs.70059","DOIUrl":"https://doi.org/10.1002/jqs.70059","url":null,"abstract":"<p>Facing a novel plague pandemic, military invasions, and political–economic transformations, societies of the eastern Roman (Byzantine) empire had to adapt to a variety of pressures and new ways of exploiting their natural environments during the mid-1<sup>st</sup> millennium CE. As a result, the rural economy of Anatolia transitioned from the intensive mixed-farming regime of the Graeco-Roman era to a more varied medieval agricultural system. We reconstruct here for the first time this transition in a region of Anatolia located close to Constantinople through pollen analysis of a sediment core from Lake Yeniçağa, dated to between ~2300 and ~1200 cal a BP. After discussing data for the Hellenistic–Roman era, we document repeated attempts at the recovery of mixed farming during the 6<sup>th</sup> to 8<sup>th</sup> c. CE. These attempts were only successful toward the end of our study period, with the stabilization of the military situation in the region, as is also visible in the written sources that we analyze in parallel in this paper. Crucially, this model of land exploitation was also constrained by the climatic oscillations that reflected its transitional location between the Aegean, Central Anatolian, and Black Sea climate regions. Thus, our study provides a perfect illustration of the interplay between environment and society in relation to the primary production sector (agriculture), in the dynamic context of a strong elite presence in the nearby capital city.</p>","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"41 3","pages":"520-539"},"PeriodicalIF":2.2,"publicationDate":"2026-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/jqs.70059","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147686896","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}
引用次数: 0
Cordilleran Ice Sheet early deglaciation inferred from evolution of Late-Pleistocene glacial Lake Dzulh Stun in east-central British Columbia, Canada 加拿大不列颠哥伦比亚省中东部晚更新世Dzulh Stun冰川湖的演化推断科迪勒兰冰盖早期消冰作用
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-02-17 DOI: 10.1002/jqs.70051
Brendan G. N. Miller, John J. Clague, Andrée Blais-Stevens
{"title":"Cordilleran Ice Sheet early deglaciation inferred from evolution of Late-Pleistocene glacial Lake Dzulh Stun in east-central British Columbia, Canada","authors":"Brendan G. N. Miller,&nbsp;John J. Clague,&nbsp;Andrée Blais-Stevens","doi":"10.1002/jqs.70051","DOIUrl":"https://doi.org/10.1002/jqs.70051","url":null,"abstract":"<p>We document the early decay of the Late-Pleistocene Cordilleran Ice Sheet in the central portion of the Rocky and Cariboo Mountains and the Rocky Mountain Trench in east-central British Columbia. Glacial lakes impounded at the eastern margin of the ice sheet occupied watersheds on the west flank of the central Rocky Mountains, leaving extensive glaciolacustrine deposits and shorelines. Some of the lakes overflowed across high divides onto the westernmost Interior Plains. These lakes expanded westward and eventually coalesced to form glacial Lake Dzulh Stun, which grew to occupy ~400 km of the Rocky Mountain Trench and extended farther west into the adjacent Cariboo Mountains. Meltwater from the margin of the ice sheet located in the central Cariboo Mountains crossed the crest of the range in places and flowed into this lake. At this time, high elevations on the east side of the Cariboo Mountains were ice-free, while major cross-cutting valleys remained obstructed by ice. The lake drained to the north along the Parsnip River valley, through the Rocky Mountains and onto the Interior Plains, accompanied by an ~400 m (1213–808 m ASL) lowering in its level. These events occurred during perhaps a millennium within the period 13–14.5 ka before present.</p>","PeriodicalId":16929,"journal":{"name":"Journal of Quaternary Science","volume":"41 3","pages":"452-472"},"PeriodicalIF":2.2,"publicationDate":"2026-04-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/jqs.70051","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"147686264","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}
引用次数: 0
Small mammal assemblages from paleosols in Eastern Europe indicate evolutionary trends and predominantly warm and dry climates across Middle and Late Pleistocene Interglacials 来自东欧古土壤的小型哺乳动物组合表明了中更新世和晚更新世间冰期的进化趋势和主要的温暖和干燥气候
IF 2.2 3区 地球科学
Journal of Quaternary Science Pub Date : 2026-04-13 Epub Date: 2026-02-18 DOI: 10.1002/jqs.70056
Anastasia K. Markova, Andrey Yu. Puzachenko, Alexander I. Tsatskin
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