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Quaternary, Volume 8, Issue 2 (June 2025) – 6 articles

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6 pages, 1311 KiB  
Article
Two Circumpolar Ground Beetle Species (Coleoptera: Carabidae) Were in Hokkaido, Japan, Late in the Last Glacial Period
by Shigehiko Shiyake
Quaternary 2025, 8(2), 22; https://doi.org/10.3390/quat8020022 - 2 May 2025
Viewed by 126
Abstract
Fossilized body parts of two cold-adapted ground beetle species, Elaphrus lapponicus and Diacheila polita, were identified from a deposit dated to the Late Glacial period in Hokkaido, Japan. The paleoenvironmental reconstruction presented here has been based on modern temperature ranges and environmental [...] Read more.
Fossilized body parts of two cold-adapted ground beetle species, Elaphrus lapponicus and Diacheila polita, were identified from a deposit dated to the Late Glacial period in Hokkaido, Japan. The paleoenvironmental reconstruction presented here has been based on modern temperature ranges and environmental conditions, along with paleobotanical evidence from the site. Late Glacial temperatures were at least 6 degrees °C lower than modern temperatures in summer, and the area around the site was mostly covered with forest tundra, which exists only in areas further north than Hokkaido. Full article
(This article belongs to the Special Issue Climate Change and Reconstruction of the Palaeoecological Changes)
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15 pages, 4669 KiB  
Article
Food Production and Landscape Reconstruction of Liangzhu Culture Village (5000–4600 B.P.)—Archaeobotanical Evidence from the Site of Zhumucun, Southern China
by Xiaoqu Zheng, Fan Yang, Mingli Sun and Qinyu Chen
Quaternary 2025, 8(2), 21; https://doi.org/10.3390/quat8020021 - 27 Apr 2025
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Abstract
Preserved macro-botanical and charcoal remains collected from the Zhumucun site have revealed the paleodiet and agricultural production of a small settlement during the Liangzhu period. Further, they have also helped to reconstruct the landscape and social organization that occurred therein. The plant remains [...] Read more.
Preserved macro-botanical and charcoal remains collected from the Zhumucun site have revealed the paleodiet and agricultural production of a small settlement during the Liangzhu period. Further, they have also helped to reconstruct the landscape and social organization that occurred therein. The plant remains assemblage shows that rice was the main crop at this site; however, the appearance of the millets may also indicate the spread and communication between southern and northern China. An analysis of the discarded spikelets confirmed that rice was locally produced and processed. A study of charcoal helped restore the vegetation landscape in the settlement and provided valuable insights for reconstructing the functional zoning and agricultural production at the site. Following an analysis of the plant distribution and utilization patterns at the site, it became clear that the Zhumucun site functioned as a small agricultural settlement. Compared to other settlements from the Liangzhu period, the Zhumucun site likely supported a smaller population. The site could be divided into smaller groups, including facilities in residential areas, processing areas, tomb areas, and farming areas. Agricultural production at the Zhumucun site appears to have been highly coordinated, with activities carried out in a unified manner and primarily by local households. This efficient system of resource management likely reflects a well-organized labor structure, where food surpluses may have been redistributed to support other higher-level settlements. Full article
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25 pages, 3420 KiB  
Article
Current Phylogeographic Structure of Anemone altaica (Ranunculaceae) on the Khamar-Daban Ridge Reflects Quaternary Climate Change in Baikal Siberia
by Marina Protopopova, Polina Nelyubina and Vasiliy Pavlichenko
Quaternary 2025, 8(2), 20; https://doi.org/10.3390/quat8020020 - 22 Apr 2025
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Abstract
Anemone altaica Fisch. ex C. A. Mey., a component of the tertiary boreo-nemoral vegetation complex, exhibits a disjunct distribution from European Russia to Central China. The Khamar-Daban Ridge, extending along Lake Baikal’s southern coast, has served as a refugium preserving mesophilic forest remnants [...] Read more.
Anemone altaica Fisch. ex C. A. Mey., a component of the tertiary boreo-nemoral vegetation complex, exhibits a disjunct distribution from European Russia to Central China. The Khamar-Daban Ridge, extending along Lake Baikal’s southern coast, has served as a refugium preserving mesophilic forest remnants in South Siberia since the Pleistocene. This study aimed to elucidate the phylogenetic relationships and historical biogeography of A. altaica within the Khamar-Daban refugium using plastid DNA markers (trnL + trnL-trnF). Phylogenetic and mismatch distribution analysis revealed polyphyly (more specifically diphyly) among A. altaica lineages, suggesting past hybridization events with related species followed by backcrossing. Estimation of isolation by distance effect, spatial autocorrelation analysis, PCoA, and AMOVA indicated a clear spatial genetic structure for A. altaica on the Khamar-Daban Ridge. The most reliable geographical model suggests that during periods of Pleistocene cooling, A. altaica persisted in at least six microrefugia within the ridge. Populations associated with these microrefugia formed western, central, and eastern genetic supergroups with limited gene flow among them. Gene flow likely occurred more easily during glaciations or early interglacials when the subalpine zone shifted closer to Lake Baikal due to the depression of the snow boundary, allowing adjacent populations to intermingle along the glacial edges and terminal moraines in mountain forest belt. Full article
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33 pages, 2340 KiB  
Article
Dietary Reconstruction of Pliocene–Pleistocene Mammoths and Elephants (Proboscidea) from Northern Greece Based on Dental Mesowear Analysis
by Christos Tsakalidis, George E. Konidaris, Evangelia Tsoukala and Dimitris S. Kostopoulos
Quaternary 2025, 8(2), 19; https://doi.org/10.3390/quat8020019 - 11 Apr 2025
Viewed by 549
Abstract
Dental wear analyses of extinct animals offer key insights into their dietary preferences and in turn contribute substantially to palaeoenvironmental reconstructions, leading to more accurate interpretations about past ecosystems. This study employs dental mesowear analysis on Pliocene and Pleistocene elephants and mammoths from [...] Read more.
Dental wear analyses of extinct animals offer key insights into their dietary preferences and in turn contribute substantially to palaeoenvironmental reconstructions, leading to more accurate interpretations about past ecosystems. This study employs dental mesowear analysis on Pliocene and Pleistocene elephants and mammoths from several localities in Northern Greece (Ptolemais Basin, Mygdonia Basin, Drama Basin, and the Neapolis-Grevena Basin), aiming to classify them into three main dietary categories (browsers, mixed-feeders, grazers) and investigate potential niche partitioning. The method relies on documenting the wear pattern of molar surfaces through angle measurements on the enamel ridges, which reflect the average annual diet of the examined taxon and in turn the annual ecological conditions of the studied area. Prior to the palaeodietary study and in order to ensure the taxonomic attribution of the examined specimens, a taxonomic review was conducted which confirmed the presence of the mammoths Mammuthus rumanus, Mammuthus meridionalis (southern mammoth), and Mammuthus trogontherii (steppe mammoth), and the European straight-tusked elephant Palaeoloxodon antiquus. Dental mesowear results indicate a grazing diet for M. (cf.) rumanus, a mainly browsing diet for M. meridionalis but mixed-feeding to grazing for the subspecies Mammuthus meridionalis vestinus, a grazing one for M. trogontherii, and a wide diet spectrum for P. antiquus, including browsing, mixed-feeding and grazing, depending on the locality. This study expands our knowledge on the palaeoecology of Greek proboscideans and further highlights the importance of mesowear analysis on proboscidean teeth for palaeodietary and palaeoenviromental inferences. Full article
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7 pages, 223 KiB  
Editorial
Palynology for Sustainability: A Classical and Versatile Tool for New Challenges—Recent Progress
by Anna Maria Mercuri, Assunta Florenzano, Eleonora Clò and Gabriel Servera-Vives
Quaternary 2025, 8(2), 18; https://doi.org/10.3390/quat8020018 - 1 Apr 2025
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Abstract
Palynology deals with several topics closely linked to sustainability [...] Full article
19 pages, 3028 KiB  
Article
Evaluation of Temperature and Precipitation Since 4.3 ka Using Palynological Data from Kundala Lake Sediments, Kerala, India
by Anjum Farooqui and Salman Khan
Quaternary 2025, 8(2), 17; https://doi.org/10.3390/quat8020017 - 1 Apr 2025
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Abstract
A comprehensive database of paleo vegetation from Kundala Lake, Kerala, was used for a palynological study in a 120 cm sedimentary profile from Kundala Lake (1700 mamsl), Palni Hills, to understand the climate and vegetation equilibrium during the last four millennia. On the [...] Read more.
A comprehensive database of paleo vegetation from Kundala Lake, Kerala, was used for a palynological study in a 120 cm sedimentary profile from Kundala Lake (1700 mamsl), Palni Hills, to understand the climate and vegetation equilibrium during the last four millennia. On the basis of pollen assemblage and cluster analysis, a relatively high percentage of evergreen vegetation between 4.3 and 3.4 ka (phase I) was inferred to represent the relicts of middle Holocene vegetation during a warmer climate. Subsequently, in the periods of 3.4–2.3 ka (phase II) and 2.3–0.87 ka (phase III), herbs/shrubs dominated. A relative increase in the percentage of arboreals along with herbaceous taxa was again observed from 0.87 to 0.12 ka (phase IV). Later, in phase V (from 1820 AD to present), few new plant taxa were recorded. On the basis of the ‘coexistence approach’, the Mean Annual Temperature (MAT) was inferred to be 22 °C, 15 °C, 15 °C, 20 °C and 22 °C during phases I to V, respectively. The Mean Annual Precipitation (MAP)was 2660 ± 3700 mm from ~4.3 to 0.12 ka; however, it decreased to ~1750 mm between 3.4 and 2.3 ka. However, pollen evidence reveals short-term cooler spells during the 16/17th century AD, which is in concordance with the globally recorded cooler and arid climate that began sometime from ~5.0 to 4.0 ka. A thematic digital elevation map of vegetation reconstructed for the years 2005 and 2018 shows a reduction in evergreen plants and water bodies in the vicinity of Kundala Lake, which was correlated with the results of palynological studies and Indian meteorological data for the last ~100 years in the region. Full article
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