Quaternary International最新文献

{"title":"Analysis of plant micro-remains and organic acid residues reveals the dietary conditions at the Chengyan site during the early Yangshao Culture in western Henan, central China","authors":"Yingxue Gong ,&nbsp;Yuzhang Yang ,&nbsp;Xingtao Wei ,&nbsp;Jingwen Liao ,&nbsp;Binggui Sun ,&nbsp;Yuchun Wang ,&nbsp;Juzhong Zhang","doi":"10.1016/j.quaint.2025.109848","DOIUrl":"10.1016/j.quaint.2025.109848","url":null,"abstract":"<div><div>The early Yangshao period (<em>ca</em>. 7.0–6.0 ka BP) is a pivotal transition stage for prehistoric human subsistence strategies from hunting and gathering to farming and husbandry. The western Henan Province constitutes the core area of Yangshao Culture. To investigate the dietary conditions of the early Yangshao ancestors in this area, analysis of plant micro-remains (starch grains and phytoliths) and organic acid residues was conducted on 34 pottery samples unearthed at the Chengyan Site in Lingbao City, western Henan Province, central China. The results revealed that the plant foods of the Chengyan people included Triticeae, Job's tears (<em>Coix lacryma-jobi</em>), rice (<em>Oryza sativa</em>), millet (<em>Setaria italica</em> and <em>Panicum miliaceum</em>), lotus root <em>(Nelumbo nucifera</em>), snake gourd root (<em>Trichosanthes kirilowii</em>), yam (<em>Dioscorea</em>), lily (<em>Lilium brownii</em>), legumes (Fabaceae), and acorn (<em>Quercus</em>), in which, some species served as raw materials for brewing fermented beverages. These findings demonstrate that botanical resource exploitation during this period in central China exhibited remarkable diversity, with foraging maintaining its significance as an essential subsistence strategy for early human populations in acquiring plant foods. The presence of rice at the Chengyan site indicates its spread to western Henan during the early Yangshao period, and a rice-millet mixed farming, dominated by foxtail millet and broomcorn millet, had developed in the area. This study provides valuable insights into the dietary patterns and agricultural production trajectories of the early Yangshao communities in the Central Plains region.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"736 ","pages":"Article 109848"},"PeriodicalIF":1.9,"publicationDate":"2025-05-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144116473","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}

{"title":"Paleoenvironmental changes and sea-level fluctuations record at Punta de s’Avançada, Mallorca Island","authors":"Federica Perazzotti ,&nbsp;Laura del Valle ,&nbsp;Giulia Cossu ,&nbsp;Vincenzo Pascucci ,&nbsp;Joan J. Fornós","doi":"10.1016/j.quaint.2025.109839","DOIUrl":"10.1016/j.quaint.2025.109839","url":null,"abstract":"<div><div>Coastal landscapes are the most sensitive system to abrupt climate changes and important archives of past changes and can be used to reconstruct possible future scenarios potentially undergoing recurrent extreme climatic events. Evidence of this change can be observed in the study area of this paper, Punta de s’Avançada in Pollença, Mallorca (Balearic Islands, Spain). The stratigraphic record from the Punta de s'Avançada outcrop in North Mallorca provides valuable insights into the paleoenvironmental changes driven by Heinrich (HE) and Dansgaard-Oeschger (DO) events during the late Pleistocene. Detailed analysis of six distinct sedimentary units (U1-U6) reveals the significant impact of abrupt climatic shifts on sediment supply, depositional environments, and sea-level fluctuations. The cold, arid conditions during HE events, particularly H4 and H5, promoted extensive dune formation in Units U4 and U6, while the warmer, wetter conditions during DO events facilitated alluvial and colluvial deposition in Units U1 and U5. By integrating OSL dating with climatic oscillations, this study demonstrates the influence of millennial-scale HE and DO events on sedimentary processes in coastal landscapes of the western Mediterranean. The results show ages between 34 and 91 ka, suggesting a time interval between MIS 3 and MIS 5a. The findings underline the dynamic interplay between climate, sea level, and sedimentation in shaping Pleistocene coastal environments, contributing to a deeper understanding of the region response to glacial cycles and abrupt climate events.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"735 ","pages":"Article 109839"},"PeriodicalIF":1.9,"publicationDate":"2025-05-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144116219","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}

{"title":"Landform basis for the rise of early cities in the upper Jialu river basin, central China","authors":"Ye Li ,&nbsp;Peng Lu ,&nbsp;Panpan Chen ,&nbsp;Hui Wang ,&nbsp;Shugang Yang ,&nbsp;Xiangli Zhao ,&nbsp;Yinan Liao ,&nbsp;Yan Tian ,&nbsp;Zhen Wang ,&nbsp;Duowen Mo","doi":"10.1016/j.quaint.2025.109842","DOIUrl":"10.1016/j.quaint.2025.109842","url":null,"abstract":"<div><div>As a significant emblem of human culture, the emergence and evolution of early cities represent a pivotal milestone in the chronicles of human history. However, the environmental mechanisms underlying the rise of early cities are still ambiguous. In this study, we conducted a comprehensive investigation of early cities and their landform basis in the upper Jialu River basin of Central China. By field surveys, OSL dating, and grain size analysis, we reconstructed the fluvial geomorphic evolution since the late Pleistocene and examined how landforms influenced the distribution of early city sites. The results showed that the water system pattern, including the Jialu River and its tributaries, had been established during the early Pleistocene. At 80-16 ka BP, there was continuous accumulation in the area. From 15 to 9.8 ka BP, the river incision resulted in the formation of the expansive T3 terrace. Between 9.8 and 2.5 ka BP, the regional geomorphology stabilized. Around 2.5 ka BP, river downcutting resulted in the formation of the T2 terrace. Following a minor accumulation phase, the T1 terrace emerged during the late historical period. The region's distinctive through-shaped landform was instrumental in the emergence and evolution of early cities. The landscape stability resulting from the river incision facilitated early urbanization and the expansion of urban areas. The river incision also fixed river channels in the plain areas, which were previously occupied by swamps and wetlands that gradually transformed into land, providing a foundation for the establishment of Zhengzhou Shang City, the capital of the early Shang Dynasty.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"735 ","pages":"Article 109842"},"PeriodicalIF":1.9,"publicationDate":"2025-05-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144107304","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}

{"title":"16,000-year hydroclimate reconstruction from Lake Von, Aotearoa New Zealand indicates Pacific-wide synchrony in Southern Hemisphere westerly wind variability","authors":"Greer Gilmer ,&nbsp;Christopher M. Moy ,&nbsp;Marcus J. Vandergoes ,&nbsp;Christina R. Riesselman ,&nbsp;William I. Henríquez","doi":"10.1016/j.quaint.2025.109826","DOIUrl":"10.1016/j.quaint.2025.109826","url":null,"abstract":"<div><div>The intensity and latitudinal position of the Southern Hemisphere westerly winds (SWW) influence precipitation patterns across the mid to high latitudes of the Southern Hemisphere, including across southern Te Waipounamu/South Island, Aotearoa New Zealand. Te Waipounamu/South Island is located along the modern northern margin of the strongest SWW, but there are no continuous high-resolution records of westerly wind variability and hydroclimate that extend back to the end of glaciation from this region. Here, we present a multi-millennial to multi-centennial reconstruction of hydroclimate and westerly wind intensity for southern Aotearoa New Zealand using a sediment core from Lake Von in Central Otago that spans the last ∼16,000 years. Higher lake levels and an expanded lake extent are caused by cooler and wetter climate conditions under more intense westerly wind flow. Conversely, a reduction in westerly wind intensity results in a warmer and drier climate, lower lake levels and migration of the shoreline towards the lake depocenter. There are seven episodes of low lake level between 11100 and 3500 cal yr BP that occur within two broad intervals between 11100 and 8300 cal yr BP and 6000–3500 cal yr BP. There are three periods of relatively high lake level between 12500 and 11200 cal yr BP, 8300 - 6000 cal yr BP, and 3500 cal yr BP to present. Multi-millennial to multi-centennial fluctuations in hydroclimate and westerly wind intensity at Lake Von are replicated by records across the Pacific Basin in southern South America showing synchronous hemisphere-wide shifts in westerly wind intensity through time.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"735 ","pages":"Article 109826"},"PeriodicalIF":1.9,"publicationDate":"2025-05-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144107294","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}

{"title":"Unravelling the enigma of wind dynamics in the Minoan eruption of Thera: Exploring the influence of wind patterns during the Late Bronze Age catastrophe","authors":"Dimitrios Ntokos","doi":"10.1016/j.quaint.2025.109838","DOIUrl":"10.1016/j.quaint.2025.109838","url":null,"abstract":"<div><div>The Minoan volcanic eruption of Thera, one of the most powerful volcanic events in recorded history, profoundly disrupted the Minoan civilization and altered the geopolitical landscape of ancient Eastern Mediterranean societies through widespread tephra deposition. This study investigates the dynamics of prevailing wind systems and their role in shaping the spatial distribution of volcanic ash during the eruption. A geospatial model employing Kriging interpolation was developed within a Geographic Information System (GIS) framework to estimate tephra dispersal patterns. The model was based on tephra thickness measurements from published site data and utilized spatial autocorrelation to interpolate deposition across unsampled regions. The results indicate that volcanic material was predominantly transported northeastward via stratospheric wind systems and southward due to northerly and northwesterly tropospheric winds over the Aegean Sea. The seasonal co-occurrence of these wind regimes, particularly during late spring, suggests that the eruption most likely occurred in May. The findings provide new insight into the atmospheric mechanisms of high-magnitude eruptions and their broader environmental and societal implications.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"735 ","pages":"Article 109838"},"PeriodicalIF":1.9,"publicationDate":"2025-05-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144084074","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}

{"title":"Holocene vegetation history of western Chukotka (Northeastern Asia) inferred from pollen records","authors":"D.V. Petrov ,&nbsp;A.A. Andreev ,&nbsp;G.K. Danilov ,&nbsp;A.A. Oskolski ,&nbsp;V.I. Tsygankova ,&nbsp;S.L. Vartanyan","doi":"10.1016/j.quaint.2025.109841","DOIUrl":"10.1016/j.quaint.2025.109841","url":null,"abstract":"<div><div>Although paleoecological studies in the high Arctic has intensified in recent decades, many regions of the northeastern Siberia remain understudied. We present 5 new Holocene pollen records from northwestern Chukotka, Northeastern Asia. These findings contribute to our knowledge of landscape transformation in the Arctic since the end of Lateglacial time and are important for climate change predictions. Study sites are located in the basin of the Yurumkuveem River, the Chaun Lowland nd the lower flow of Pegtymel’ River. The results indicate, that the climatic conditions in the Early Holocene were more favorable for the local vegetation than those of today. The lower reaches of the Pegtymel’ River were occupied by southern tundra; several woody plant species grew in the river valleys of the Chaun Lowland, while larch accompanied by poplar and chosenia gallery forests reached Nyrki Lake the in northern part of the Anadyr River basin. With the onset of the Mid Holocene, trees and shrubs began to gradually disappear from the local vegetation communities indicating a climatic deterioration. Modern like vegetation was established in study region at the beginning of the Late Holocene.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"733 ","pages":"Article 109841"},"PeriodicalIF":1.9,"publicationDate":"2025-05-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144069722","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}

{"title":"MIS3 – MIS2 transition based on small mammal faunas from Palaeolithic sites in the centre of the East European Plain","authors":"Anastasia K. Markova,&nbsp;Andrey Yu. Puzachenko","doi":"10.1016/j.quaint.2025.109830","DOIUrl":"10.1016/j.quaint.2025.109830","url":null,"abstract":"<div><div>Palaeontological methods, including the study of fossil small mammals (Lagomorpha, Rodents, Eulipotyphla), are instructive for paleoenvironmental reconstructions. This paper presents results of fossil small mammals' investigation in cultural layers of six Late Pleistocene sites related to Middle and Upper Palaeolithic. In addition to prehistoric sites at Betovo, Khotylevo 2, Eliseevichi 2, Yudinovo, Novgorod Severskaya, and Byki 7, we analyse two synchronous Late Pleistocene natural faunal localities in Arapovichi and Troitsa 2, all in the centre East European Plain. The main aim of this paper is to reconstruct the transition of the regional small mammal fauna from the end of MIS 3 (the so-called Bryansk = Denekamp Interstadial) to the Last Glacial Maximum (LGM) of Marine Isotope stage 2 (MIS2) (∼32–17 ka BP). All small mammal assemblages show low species richness (3–16 taxa), with cold adapted tundra and steppe animals dominating, while forest mammals are rare or practically absent. Palaeozoological data indicate the existence of mosaic periglacial landscapes in the area, such as complicate composition of shrub tundra-like and periglacial steppe. The three-dimensional descriptive model reproduces changes in local faunal (LF) composition caused by the general climate trend during the transition from interstadial conditions at the end of MIS3 to the extremely cold conditions of the LGM (mid-MIS2). We distinguish four main phases of this transformation: phase I that corresponds to the end of MIS3 and the beginning of MIS2 and is characterised by the dominance of <em>Dicrostonyx</em> sp., relatively low occurrence of <em>Lasiopodomys anglicus/gregalis</em>, low occurrence of <em>Ochotona pusilla</em>; the next phase II is characterised by some decrease of <em>Dicrostonyx</em> sp. remains but the increase of <em>L. gregalis</em>. Phase III corresponds to the most severe climatic conditions in the GS-2.1 stadial. The youngest fauna of the Yudinovo site is characterised by the dominance of the collared lemming and the narrow-headed vole and corresponds to phase IV and the end of the LGM.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"733 ","pages":"Article 109830"},"PeriodicalIF":1.9,"publicationDate":"2025-05-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143942274","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}

{"title":"Pollen preservation evidence from southern Patagonia (52°–54°S): Old methods, new insights into past changes in the Southern Hemisphere westerly winds","authors":"Robert D. McCulloch ,&nbsp;Mary B. McCulloch","doi":"10.1016/j.quaint.2025.109825","DOIUrl":"10.1016/j.quaint.2025.109825","url":null,"abstract":"<div><div>The analysis of pollen preservation data to support the interpretation of palynological records has been recognised since the 1960s, but the method, which incurs no additional resources, has rarely been adopted in Patagonia. This paper presents a synthesis of records of palaeovegetation and pollen preservation from six peat bogs, along a latitudinal transect in southern Patagonia (51°–54°S). The peat bogs are closed basins and thus sensitive to changes in precipitation and we detail how pollen preservation data demonstrate a high degree of sensitivity to and provide a robust indicator of persistent changes in mire surface wetness (MSW). We discuss how reconstructing the changing vegetation patterns coupled with MSW, in association with other regional proxies support inferences concerning latitudinal shifts in the southern westerly winds (SWWs), an important component of the Southern Hemisphere ocean-atmosphere circulation system. We also illustrate how analysing pollen preservation data can provide more nuanced site specific and regional information on lags and threshold responses in vegetation communities, to climate changes.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"733 ","pages":"Article 109825"},"PeriodicalIF":1.9,"publicationDate":"2025-05-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143937902","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}

{"title":"Pleistocene murid rodent fossils from Semadong Cave in northern Peninsular Malaysia: taxonomic, zoogeographic, and environmental implications","authors":"Satapat Kumpitak ,&nbsp;Ros Fatihah Muhammad ,&nbsp;Lim Tze Tshen ,&nbsp;Kantapon Suraprasit","doi":"10.1016/j.quaint.2025.109805","DOIUrl":"10.1016/j.quaint.2025.109805","url":null,"abstract":"<div><div>The new fossil site of Semadong Cave in Perlis State, Malaysia, has yielded a very rich array of small vertebrate fossils that are composed mainly of fragmentary craniodental and postcranial remains of murine rodents plus some fragments of insectivores, large mammals, and amphibians. Here, we describe 383 dental remains of fossil murine rodents recovered from the whitish-grey silty clay, the fossiliferous layer deposited in the cave of Semadong. The fossil rodent assemblage is composed of ten identified murine species within seven genera, including two globally (<em>Prohadromys varavudhi</em> and <em>Saidomys siamensis</em>), and six locally <em>(Hadromys humei</em>, <em>Bandicota savilei</em>, <em>Berylmys berdmorei</em>, <em>Rattus andamanensis</em>, <em>Mus</em> cf. <em>pahari</em>, and <em>Mus cervicolor</em>) extinct taxa, two living species (<em>Rattus argentiventer</em> and <em>Rattus rattus</em>), and numerous remains identified as belonging to <em>Rattus</em> sp. and an indeterminate murine. The most abundant specimens were <em>Bandicota savilei</em>, followed by the indeterminate murine and <em>Rattus rattus</em>. The taxonomic results provide age estimates of the Pleistocene for micromammal fossil deposits. The presence of two primitive murid rodent species demonstrates the widespread distribution of Indochinese elements, extending further south of the Isthmus of Kra, into northern Sundaland. Paleoenvironmental evidence based on the presence of <em>Bandicota savilei</em>, <em>Rattus argentiventer</em>, and <em>Mus cervicolor</em> suggests that the expansion of Pleistocene tropical grasslands might have played a key role in facilitating their southward distribution. Meanwhile, other species, such as <em>Hadromys humei</em>, indicate the existence of forested areas under drier and cooler conditions than those found today.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"732 ","pages":"Article 109805"},"PeriodicalIF":1.9,"publicationDate":"2025-05-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143932060","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}

{"title":"Temperature variability in northeastern China over the Past 2000 Years: Linkages with the Arctic oscillation and solar activity","authors":"Nan Zhan ,&nbsp;Fangang Zeng ,&nbsp;Qi Li ,&nbsp;Manman Xie ,&nbsp;Ruixia Hao ,&nbsp;Li Pingping ,&nbsp;Ruilin Wen ,&nbsp;Luo Wang ,&nbsp;Qing Sun ,&nbsp;Guoqiang Chu","doi":"10.1016/j.quaint.2025.109829","DOIUrl":"10.1016/j.quaint.2025.109829","url":null,"abstract":"<div><div>Understanding regional paleotemperature changes over the past 2000 years is crucial for global climate networks, as it provides valuable insights into climate dynamics and offers a regional perspective within the global system. In this study, we present a high-resolution temperature reconstruction (∼10-year resolution) for the past two millennia, using branched dialkyl glycerol tetraethers (brGDGTs) from the laminated sediments of Lake Shuanggoushan in Northeast China. Our reconstruction of month-above-freezing temperatures (MAFT) revealed significant temperature variability on decadal to centennial timescales, which aligns well with other paleotemperature records from Northeast China but diverges from the composite temperature series of the broader Chinese region. In this region, instrumental records revealed a strong positive correlation between the Arctic Oscillation (AO) and winter-spring temperatures (Nov–Apr), with a weaker correlation during the ice-free season (May–Oct). Paleoclimate records further demonstrate a weak positive correlation (r = 0.22, p &lt; 0.01) between the AO index and MAFTs on decadal timescales, suggesting that the AO has influenced regional temperature variability over the past 2000 years. Spectral analysis of the temperature time series identified two periodicities (55–57 and 66–67 years) with 99 % confidence, which closely align with the ∼60-year solar cycle. This finding indicated a possible link between temperature variability and solar activity. Overall, our results highlight the significance of the AO and solar activity in driving decadal temperature variability during ice-free seasons in Northeast China over the past two millennia.</div></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"733 ","pages":"Article 109829"},"PeriodicalIF":1.9,"publicationDate":"2025-05-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143928210","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}