Quaternary International最新文献

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A pollen-based reconstruction of middle to late holocene precipitation dynamics in Anyang archaeological area, Central Plains, China 基于花粉的中国中原安阳考古区全新世中晚期降水动态重建
IF 2.2 3区 地球科学
Quaternary International Pub Date : 2024-06-04 DOI: 10.1016/j.quaint.2024.05.014
Songna Wang , Xiaodong Miao , Zhengchuang Hui , Zijuan Yong , Tianyu Shi
{"title":"A pollen-based reconstruction of middle to late holocene precipitation dynamics in Anyang archaeological area, Central Plains, China","authors":"Songna Wang ,&nbsp;Xiaodong Miao ,&nbsp;Zhengchuang Hui ,&nbsp;Zijuan Yong ,&nbsp;Tianyu Shi","doi":"10.1016/j.quaint.2024.05.014","DOIUrl":"10.1016/j.quaint.2024.05.014","url":null,"abstract":"<div><p>In the context of global warming, the dynamics of East Asian Summer Monsoon (EASM) are of great significance for predicting future climate change. The variations of humidity indicated by various climate proxies in Central China are controversial. This study relies on pollen data retrieved from lacustrine sediment at the Anshang site in Anyang archaeological area, Central Plains of China to quantitatively reconstruct the change in PANN (mean annual precipitation). The results show that the region experienced three distinct dry-wet intervals during the ∼8.54 to ∼3.26 cal ka BP: the earlier portion of the mid-Holocene (∼8.5–∼6.0 cal ka BP) witnessed the higher PANN; the latter portion of the mid-Holocene (∼6.0–∼3.6 cal ka BP) enjoyed the highest PANN of the past ∼8500 years with a noticeable cold and dry event occurred around 4.2 cal ka BP; the late Holocene (∼3.6–∼3.2 cal ka BP) experienced the lower PANN. Periodic analysis on pollen-based precipitation further reveals ∼500-year and ∼800-year cycles, matching well with regional climate records. Our regional comparison suggests that the Central Plains of China shared similar climatic controls with the southern region of China during the ∼8.54 to ∼3.26 cal ka BP. Shifts of Western Pacific Subtropical High (WPSH), driven by the ENSO (El Niño-Southern Oscillation) conditions and SST (Sea Surface Temperatures) in the western tropical Pacific, regulated the positioning of the EASM-related rain-belt during ∼8.54 to ∼3.26 cal ka BP. This study provides more reliable variations of humidity in the Central Plains under the influence of the EASM, which is helpful to predict future climate change.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":2.2,"publicationDate":"2024-06-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141274591","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
Late Quaternary bioerosion pattern controlled by upwelling events at Puerto Lobos (Chubut, Argentina) 第四纪晚期生物侵蚀模式受 Puerto Lobos(阿根廷丘布特)上升流事件控制
IF 2.2 3区 地球科学
Quaternary International Pub Date : 2024-05-31 DOI: 10.1016/j.quaint.2024.05.009
Luciana M. Giachetti , Sebastián Richiano , Diana E. Fernández , Clara B. Giachetti
{"title":"Late Quaternary bioerosion pattern controlled by upwelling events at Puerto Lobos (Chubut, Argentina)","authors":"Luciana M. Giachetti ,&nbsp;Sebastián Richiano ,&nbsp;Diana E. Fernández ,&nbsp;Clara B. Giachetti","doi":"10.1016/j.quaint.2024.05.009","DOIUrl":"https://doi.org/10.1016/j.quaint.2024.05.009","url":null,"abstract":"<div><p>Bioerosion traces are a powerful tool for reconstructing benthic paleo-communities through the geological record. The late Quaternary marine deposits of Patagonia (Argentina) are elongated ridges parallel to the present coast, rich in sand, gravel and shells, the latter being the main substrate for bioerosion traces. However, the ichnological studies in the Quaternary are scarce in high latitudes of the Southern Hemisphere. This work describes for the first time the bioerosion traces recorded in shells belonging to diverse taxa of mollusc from Quaternary deposits in Puerto Lobos, Southern of San Matias Gulf (Patagonia, Argentina). This study complements the scarce information on bioerosion traces in the Southern Hemisphere. A total of 710 mollusc shells were obtained from four Quaternary beach ridges at Puerto Lobos. As a result, 15 ichnotaxa were recorded for the first time in the site, 13 of them for the first time in the Holocene of San Matías Gulf. Through qualitative analysis, bioerosion patterns were observed in the late Quaternary of Puerto Lobos. The abundance of worm and sponge borings in the Pleistocene could be related to warm and sediment-free waters. On the contrary, the results of the bioerosion study in the Holocene and recent samples were very similar. This could indicate that the same environmental factor controlled both bioerosion patterns. For the Holocene, it was observed that the bioerosion pattern is mainly represented by trace produced by suspension and filter-feeding organisms, such as bryozoans, among others. Together with the increase in ichnodiversity, this could indicate an increase in nutrient availability in the San Matías Gulf associated with upwelling events. Therefore, our results reinforce the hypothesis proposed by previous authors that the upwelling events currently observed in the study area began during the mid-Holocene.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":2.2,"publicationDate":"2024-05-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141323975","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
The timber trade in the Vesuvian area before 79 AD as inferred from dendrochronological research at Moregine site 从莫雷金遗址的树木年代学研究推断出的公元 79 年前维苏威地区的木材贸易情况
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-05-30 DOI: 10.1016/j.quaint.2024.05.011
{"title":"The timber trade in the Vesuvian area before 79 AD as inferred from dendrochronological research at Moregine site","authors":"","doi":"10.1016/j.quaint.2024.05.011","DOIUrl":"10.1016/j.quaint.2024.05.011","url":null,"abstract":"<div><p>The substantial volume of timber recovered from the aftermath of the eruption of Vesuvius in 79 AD offers a valuable resource for gaining insights into the timber trade during Roman times. Silver fir emerges as the dominant species in construction within the Vesuvian region. While this species once thrived more abundantly along the Apennines, it now exists only in small, isolated groups, raising the possibility that the Romans contributed to its scarcity. Nevertheless, the origins of the substantial quantity of silver fir wood discovered in Pompeii, Herculaneum, and the surrounding areas remain unclear. This study examines 35 wood samples obtained during the excavation of the Moregine site, an ancient commercial port located a mere 600 m to the south of Pompeii's walls. Dendrochronological analysis successfully dated 19 out of the 35 samples. Despite silver fir not being the ideal species for dendroprovenancing analysis, certain observations can be made regarding its likely foreign origin. The correlation with chronologies of different species of Central European origin, the presence of species such as spruce/larch among the structural material and the existence of different groups among the material analysed are strong indications that demonstrate the foreign origin of at least some of the timber. Dendrochronological data further support that the wood trade played a strategically significant role in the economy of ancient Rome.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":1.9,"publicationDate":"2024-05-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S1040618224001733/pdfft?md5=73ef021d34a9d1071c86e6041be7c437&pid=1-s2.0-S1040618224001733-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142173638","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
Reconstructing hypoxia on the eastern Arabian sea continental shelf during the past ∼7400 years: A multi-proxy approach 重建过去∼7400年间阿拉伯海东部大陆架的缺氧状况:多代理方法
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-05-24 DOI: 10.1016/j.quaint.2024.05.007
{"title":"Reconstructing hypoxia on the eastern Arabian sea continental shelf during the past ∼7400 years: A multi-proxy approach","authors":"","doi":"10.1016/j.quaint.2024.05.007","DOIUrl":"10.1016/j.quaint.2024.05.007","url":null,"abstract":"<div><p><span><span>Shallow-sea environmental variations in the eastern Arabian Sea (EAS) have been related to monsoon variability, poorly ventilated intermediate water, and primary productivity changes. To understand these conditions, benthic foraminiferal assemblages, </span>oxygen isotope ratios<span><span>, and total organic carbon content have been examined in </span>sediment Core<span> SK291/GC13 from the EAS. We aim to retrieve decadal to centennial time-scale changes in past oxygenation and paleoproductivity during the last 7400 calibrated years before the present (cal yr BP). Our proxy data suggest that the oxic </span></span></span>benthic foraminifera<span> species were dominant during ∼7400–6000 cal yr BP. The change from oxic to dysoxic occurred during ca. 6000–3500 cal yr BP, and transition from dysoxic to suboxic environmental conditions happened at ca. ∼3500 cal yr BP. These changes are contemporaneous with weakening of the Indian summer monsoon<span><span> beginning at ∼5500 cal yr BP which culminated into a major arid phase so-called ca 4.2 ka event in the Indian subcontinent<span><span>. The EAS experienced low productivity during the early phase of our studied interval (∼7400–6000 cal yr BP) and higher productivity in the middle Holocene<span> (6000–3000 cal yr BP), as revealed by the total organic carbon and benthic assemblages. Furthermore, productivity increased in the warm period and decreased in the </span></span>Little Ice Age on a decadal scale. The spectral analysis of total organic content and suboxic species indicates a 23-year Hale (solar) cycle during the last millennium, indicating a close relationship between solar activity and monsoon variability. The strengthening of the El Nino-Southern Oscillation perhaps amplified due to increased solar activity in the last millennium, which influenced the climate of the EAS. The study highlights paleo-oxygenation shifts based on benthic foraminiferal assemblages, which are crucial for understanding changes in the oxygen minimum zones (OMZs) and their potential impacts on </span></span>marine ecosystems.</span></span></p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":1.9,"publicationDate":"2024-05-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141144034","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
Expedient Bayesian prediction of subfossil bone protein content using portable ATR-FTIR data 利用便携式 ATR-FTIR 数据对亚化石骨蛋白质含量进行贝叶斯快速预测
IF 2.2 3区 地球科学
Quaternary International Pub Date : 2024-05-18 DOI: 10.1016/j.quaint.2024.05.002
Sean Hixon , Patrick Roberts , Ricardo Rodríguez-Varela , Anders Götherström , Elena Rossoni-Notter , Olivier Notter , Pauline Raimondeau , Guillaume Besnard , Enrico Paust , Mary Lucas , Anna Lagia , Ricardo Fernandes
{"title":"Expedient Bayesian prediction of subfossil bone protein content using portable ATR-FTIR data","authors":"Sean Hixon ,&nbsp;Patrick Roberts ,&nbsp;Ricardo Rodríguez-Varela ,&nbsp;Anders Götherström ,&nbsp;Elena Rossoni-Notter ,&nbsp;Olivier Notter ,&nbsp;Pauline Raimondeau ,&nbsp;Guillaume Besnard ,&nbsp;Enrico Paust ,&nbsp;Mary Lucas ,&nbsp;Anna Lagia ,&nbsp;Ricardo Fernandes","doi":"10.1016/j.quaint.2024.05.002","DOIUrl":"10.1016/j.quaint.2024.05.002","url":null,"abstract":"<div><p>Rapid and minimally destructive methods for estimating the endogenous organic content of subfossil bone save time, lab consumables, and valuable ancient materials. Fourier transform infrared (FTIR) spectroscopy is an established method to estimate bone protein content, and portable spectroscopes enable field applications. We review the ability of benchtop and portable FTIR indices to predict %N and %collagen from 137 bone specimens drawn from eight taxa. We also explore associations of these indices with the endogenous DNA content estimated for 105 specimens. Bulk bone elemental abundance and crystallinity index data reflect diagenetic alteration of these specimens, which come from a variety of depositional environments in four countries (Madagascar, Greece, Monaco, and Germany). Infrared (IR) indices from benchtop and portable units perform similarly well in predicting observed sample N content and collagen yields. Samples that include little collagen (0–5 wt%) tend to have similar IR index values, and we present a Bayesian approach for the prediction of collagen yields. Bone type best explains variation in target species DNA content (endogenous DNA being particularly abundant in petrosals), but low IR index values were consistently associated with minimal DNA content. We conclude that, although portable FTIR fails to distinguish collagen preservation among poorly preserved samples, a simple approach with minimal sample preparation can effectively screen bone from a variety of taxa, elements, and environments for the extraction of organics.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":2.2,"publicationDate":"2024-05-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S1040618224001496/pdfft?md5=f23dda72ee048e370cde4d448511940a&pid=1-s2.0-S1040618224001496-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141133237","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
Early Holocene inundation of Doggerland and its impact on hunter-gatherers: An inundation model and dates-as-data approach 全新世早期多格尔兰的淹没及其对狩猎采集者的影响:淹没模型和日期即数据方法
IF 2.2 3区 地球科学
Quaternary International Pub Date : 2024-05-17 DOI: 10.1016/j.quaint.2024.05.006
P.W. Hoebe , K.M. Cohen , F.S. Busschers , S. van Heteren , J.H.M. Peeters
{"title":"Early Holocene inundation of Doggerland and its impact on hunter-gatherers: An inundation model and dates-as-data approach","authors":"P.W. Hoebe ,&nbsp;K.M. Cohen ,&nbsp;F.S. Busschers ,&nbsp;S. van Heteren ,&nbsp;J.H.M. Peeters","doi":"10.1016/j.quaint.2024.05.006","DOIUrl":"10.1016/j.quaint.2024.05.006","url":null,"abstract":"<div><p>Sea-level rise was a key factor changing environments during the Early Holocene in Northwest Europe. It affected Mesolithic hunter-gatherer communities by inundating large areas in the current North Sea, commonly referred to as Doggerland. In this paper we present novel inundation models for the southern North Sea providing visualisations of lateral inundation driven by sea-level rise and relate it to frequency analysis of radiocarbon dates from archaeological sites. These improve on previous studies that relied on bathymetric data, which includes post-inundation overprints of Holocene sedimentation and erosion, and thus significantly underestimates the timing of inundation in some areas.</p><p>We constructed a paleoDEM (a composite elevation grid of the top of the Pleistocene) for the eastern part of the southern North Sea; and sea level surfaces that combine relative sea-level curves from glacio-isostatic adjustment models optimised for Britain and southern Scandinavia respectively. We corrected our paleoDEMs for tectonic background basin subsidence, and in the inundation modelling account for pre-compaction elevation of peat in coastal areas. We evaluated the impact of these model components on our results and describe the possible inundation history of Doggerland. We suggest earlier inundation than predicted by previous models, showing significant area loss around 10.5–10 ka cal BP.</p><p>Palaeogeographic changes are compared with archaeological radiocarbon data using a dates-as-data approach. Composite Kernel Density Estimate and permutation tested Summed Probability Distributions are used as a proxy for the visibility, nature and intensity of human activity. Results indicate key periods of growth and decline recorded in the dataset, as well as regional differences in growth rate, some correlating with inundation phases. Chiefly, we find elevated growth rates around 10.5–10 ka in northwest Germany and the Netherlands, contemporaneous with the abovementioned phase of extensive area loss, and moreover, with changes in culture and practices on Early Mesolithic sites.</p><p>However, the spatiotemporal distribution of archaeological data is significantly influenced by accessibility and preservation of sediments of a certain age. We discuss the importance of inundation modelling and sediment data in understanding how landscape taphonomy affects archaeological patterning, especially in dates-as-data approaches.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":2.2,"publicationDate":"2024-05-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S1040618224001538/pdfft?md5=3a888189f14cac8e2aa0037d2b8bd5a7&pid=1-s2.0-S1040618224001538-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141052902","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
Stadial and interstadial deposits of Late Nemunas (Late Weichselian/MIS 2) glaciation in south Lithuania and their interpretation 立陶宛南部内穆纳斯晚期(魏克伦晚期/MIS 2)冰川期的层积和层间沉积及其解释
IF 2.2 3区 地球科学
Quaternary International Pub Date : 2024-05-17 DOI: 10.1016/j.quaint.2024.05.003
Violeta Pukelytė, Laura Gedminienė, Valentinas Baltrūnas, Bronislavas Karmaza
{"title":"Stadial and interstadial deposits of Late Nemunas (Late Weichselian/MIS 2) glaciation in south Lithuania and their interpretation","authors":"Violeta Pukelytė,&nbsp;Laura Gedminienė,&nbsp;Valentinas Baltrūnas,&nbsp;Bronislavas Karmaza","doi":"10.1016/j.quaint.2024.05.003","DOIUrl":"10.1016/j.quaint.2024.05.003","url":null,"abstract":"<div><p>This paper presents sedimentological and paleobotanical studies of the deposits from Last Glaciation (Late Nemunas, Late Weichselian) in the middle reaches of the River Nemunas in southern Lithuania. Spores, pollen, and other palynomorphs in the intercalated sediments between the diamicton (glacial till) beds were analyzed, and the paleogeographical and paleoclimatic conditions of their sedimentation were assessed using the modern analog technique (MAT). The two till layers from the Last Glaciation, characterized by significant differences in their composition, testify to a difference in glacier movement paths in the region. The continuous sedimentation process between glacial tills provides evidence of global climate changes during the Last Glaciation and the restructuring of glacial lobes during deglaciation in the southeastern part of the Scandinavian Ice Sheet. The sedimentation process and vegetation composition bear witness to an open landscape of steppe-tundra, scattered wooded areas, and the emergence of thermophilic vegetation afterward, suggesting increased annual temperatures and higher humidity. The available data enable the identification of the Balbieriškis interstage period within the Late Nemunas Glaciation (Upper Nemunas Formation) between the Grūda and Baltija stages (Grūda and Baltija subformations) in the regional Quaternary stratigraphic scheme. This period correlates with the Marine Isotope Stage 2 (MIS 2).</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":2.2,"publicationDate":"2024-05-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141036719","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
Lithic projectile technology in the western Late Epigravettian: The case study of north-eastern Italy 西部上古晚期的石器投射技术:意大利东北部案例研究
IF 2.2 3区 地球科学
Quaternary International Pub Date : 2024-05-10 DOI: 10.1016/j.quaint.2024.04.006
Nicolò Fasser , Davide Visentin , Rossella Duches , Marco Peresani , Federica Fontana
{"title":"Lithic projectile technology in the western Late Epigravettian: The case study of north-eastern Italy","authors":"Nicolò Fasser ,&nbsp;Davide Visentin ,&nbsp;Rossella Duches ,&nbsp;Marco Peresani ,&nbsp;Federica Fontana","doi":"10.1016/j.quaint.2024.04.006","DOIUrl":"10.1016/j.quaint.2024.04.006","url":null,"abstract":"<div><p>Projectile implements are one of the most frequent transformed lithic blanks within the Upper Paleolithic assemblages. Since the first taxonomic studies, their morphological variability has been used as primary fossil director to define specific regional trends and diachronic phases. However, an exhaustive analysis of manufacturing methods and techniques applied to shape this gear category is extremely rare. In fact, during the Late Epigravettian, except for a certain typological variability, the lack of detailed studies resulted in an apparent homogeneity in armatures production. In this paper, a technological and traceological approach applied to reconstruct the whole <em>chaîne opératoire</em> of armatures manufacture in three Northern Italian sites dated between 17,000 and 12,000 cal BP demonstrates important variations in how projectile implements are fashioned, concerning shape, production methods and retouch techniques. Moreover, a large-scale comparison suggests how renewals in projectile implements production in North-Eastern Italy may result from long-distance connections between human groups over the western Late Epigravettian territory.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":2.2,"publicationDate":"2024-05-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141049589","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
Late Holocene vegetation diversity change and potential response to climate variations on the northern Qinghai-Tibetan Plateau 青藏高原北部全新世晚期植被多样性变化及对气候变化的潜在响应
IF 2.2 3区 地球科学
Quaternary International Pub Date : 2024-05-02 DOI: 10.1016/j.quaint.2024.04.008
Yueqi Zhang, Yongbo Wang, Xingqi Liu
{"title":"Late Holocene vegetation diversity change and potential response to climate variations on the northern Qinghai-Tibetan Plateau","authors":"Yueqi Zhang,&nbsp;Yongbo Wang,&nbsp;Xingqi Liu","doi":"10.1016/j.quaint.2024.04.008","DOIUrl":"10.1016/j.quaint.2024.04.008","url":null,"abstract":"<div><p>Biodiversity change under current global warming scenario has attracted wide attentions, representing general stability and balance in ecosystems. Understanding the temporal patterns and potential driving mechanisms of biodiversity changes would provide significant knowledge for ecosystem sustainability, which requires necessary investigations on long-term records during the late Holocene. The high elevation and specific environment on the Qinghai-Tibetan Plateau (QTP) promote the development of fragile alpine ecosystems, responding sensitively to regional climate variations. Based on a high-resolution fossil pollen record retrieved from Lake Kusai on the northern QTP, late Holocene vegetation diversities were estimated based on the Hill number indices, which were subsequently evaluated at three time scales, i.e., millennial, centennial and multi-decadal time scales. The results indicate that Hill number indices could represent vegetation diversity changes on the northern QTP. Reconstructed vegetation diversity indices indicate gradual variations on millennium scale in each diversity index, along with different responses to environmental factors of regional moisture and total solar irradiance. On the centennial time scale, high consistencies were identified among the vegetation diversity indices as well as correlations with environmental factors, revealing overall positive responses between diversity variations and environmental changes. Rather complicated correspondences to environmental factors appeared on the multi-decadal scale, showing different patterns in diversity indices, which illustrates variations through time as well. Accordingly, vegetation diversity changes of the alpine communities on the northern QTP experienced serious variations during the late Holocene, and revealed complicated responses to regional environmental changes, that further investigations particularly at different time scales would be necessary in the future.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":2.2,"publicationDate":"2024-05-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141038323","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
Exploring ten thousand years of variation in weapons technologies: A diachronic analysis of lithic projectile points in the puna de atacama (northern Chile) 探索武器技术的万年变迁:对阿塔卡马地区(智利北部)石质射弹点的异时空分析
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-05-01 DOI: 10.1016/j.quaint.2024.04.005
{"title":"Exploring ten thousand years of variation in weapons technologies: A diachronic analysis of lithic projectile points in the puna de atacama (northern Chile)","authors":"","doi":"10.1016/j.quaint.2024.04.005","DOIUrl":"10.1016/j.quaint.2024.04.005","url":null,"abstract":"<div><p>This article presents an analysis of the functional design of a collection of 346 projectile points from archaeological sites in the Puna de Atacama (21.9°–24.7° S) that belong to the cultural sequence dating from 12,500–2400 yr BP, which ranges from the earliest groups to inhabit the area to the emergence of the first agro-pastoralist societies. The results obtained reveal significant changes in projectile or weapons technologies throughout the sequence. This begins with projectile points whose measurements point to the predominance of the spearthrower-dart system during the Early Archaic, followed by the diversification and specialization of these technologies during the Middle Archaic, with a significant increase in the use of throwing and thrusting spears. In the Late Archaic, projectile point dimensions diminished significantly, displaying patterns that remained until the Early Formative. Nevertheless, during this last period some measurements decreased slightly, and a major change is detected in the haft width of stemmed points. Three alternate hypotheses are proposed for these last changes: 1) the presence of the bow-and-arrow system from the late Archaic onward; 2) the appearance of the bow-and-arrow system from the Early Formative only; 3) the reduction and standardization of spearthrower-darts, without the presence of the bow-and-arrow system until after the Early Formative. We argue that the first two hypotheses are the most plausible, although we consider the first to be the most likely.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":null,"pages":null},"PeriodicalIF":1.9,"publicationDate":"2024-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141053720","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}
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