Quaternary International最新文献

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Becoming Roman: The role of biological resources in the expansion of new economic and cultural models throughout the empire 成为罗马人:生物资源在新经济和文化模式扩展到整个帝国过程中的作用
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-30 DOI: 10.1016/j.quaint.2024.07.010
João Pedro Tereso, Cleia Detry, Filipe Vaz, Silvia Valenzuela-Lamas, Leonor Peña-Chocarro
{"title":"Becoming Roman: The role of biological resources in the expansion of new economic and cultural models throughout the empire","authors":"João Pedro Tereso, Cleia Detry, Filipe Vaz, Silvia Valenzuela-Lamas, Leonor Peña-Chocarro","doi":"10.1016/j.quaint.2024.07.010","DOIUrl":"10.1016/j.quaint.2024.07.010","url":null,"abstract":"","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"699 ","pages":"Pages 1-3"},"PeriodicalIF":1.9,"publicationDate":"2024-07-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142011848","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 animal remains from Calle Almendralejo nr. 41 (Mérida, Spain): A contribution to our understanding of animal husbandry in the capital of Roman Lusitania Calle Almendralejo nr.41(西班牙梅里达)的动物遗骸:有助于我们了解罗马卢西塔尼亚首都的畜牧业
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-30 DOI: 10.1016/j.quaint.2024.05.004
Cleia Detry , Macarena Bustamante-Álvarez , Francisco Javier Heras Mora
{"title":"The animal remains from Calle Almendralejo nr. 41 (Mérida, Spain): A contribution to our understanding of animal husbandry in the capital of Roman Lusitania","authors":"Cleia Detry ,&nbsp;Macarena Bustamante-Álvarez ,&nbsp;Francisco Javier Heras Mora","doi":"10.1016/j.quaint.2024.05.004","DOIUrl":"10.1016/j.quaint.2024.05.004","url":null,"abstract":"<div><p>The study of zooarchaeological collections from Mérida is still rare, lacking above all information on the Romans diet and animal management. Here we present the description of the fauna found in a dump next to the northern part of the Roman wall, which also includes some contexts of ritual nature, dated to the 1st century AD until the beginning of 5th century AD. The osteological remains of animals have shown that most of them come from food waste and worked bones. We can see that there is a temporal evolution in the use of that space and in the species used, with smaller animals being preferred in the first phase and cattle being more abundant in the 4th century. Some improvement indicators were also identified, as would be expected for a provincial capital, such as <em>Emerita Augusta</em>. Also, ritual burials of numerous dogs as well as a skeleton of the oldest specimen in Iberia of Egyptian mongoose, camel and an edible dormouse, constitute interesting discoveries in this assemblage, demonstrating that this is an exceptional sample.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"699 ","pages":"Pages 65-83"},"PeriodicalIF":1.9,"publicationDate":"2024-07-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S1040618224001514/pdfft?md5=5448d169b56bbeaa00d90bbd7df3e284&pid=1-s2.0-S1040618224001514-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142011849","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
Paleolandscape evolution along the coasts of the Baixo Alentejo (Portugal) during the Quaternary 第四纪期间葡萄牙 Baixo Alentejo 海岸的古地貌演变
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-23 DOI: 10.1016/j.quaint.2024.07.006
J.L. Goy , E. Roquero , C. Zazo , D. Moura , C.J. Dabrio , T. Boski , A. Martínez-Graña , J. Lario , T. Bardají
{"title":"Paleolandscape evolution along the coasts of the Baixo Alentejo (Portugal) during the Quaternary","authors":"J.L. Goy ,&nbsp;E. Roquero ,&nbsp;C. Zazo ,&nbsp;D. Moura ,&nbsp;C.J. Dabrio ,&nbsp;T. Boski ,&nbsp;A. Martínez-Graña ,&nbsp;J. Lario ,&nbsp;T. Bardají","doi":"10.1016/j.quaint.2024.07.006","DOIUrl":"10.1016/j.quaint.2024.07.006","url":null,"abstract":"<div><p><span><span><span>A detailed geomorphological mapping<span> allowed to understand the complex relationships interplayed between local tectonics and sedimentation across the coastal area of the Baixo Alentejo (Portugal) all along the Quaternary. Different outcrops of coastal sediments between Sines and Vilanova de Milfontes permitted to reconstruct a general sequence of up to fifteen stair-cased </span></span>marine terraces<span>, while wide sequences of alluvial fans develop in the hinterland. The distinct geomorphological disposition of these alluvial fans together with the presence/absence of marine terraces, have allowed to define different phases of paleolandscape evolution based both in </span></span>sea level changes<span> and differential uplift. A dune system has been attributed to MIS 5e in basis of OSL, and </span></span><sup>14</sup><span>C and U-series dating permitted the adscription of a beach unit to MIS 5. These data allowed to stablish the relative chronology of the entire marine terrace sequence and to determine the vertical movement rates along the studied coastal area. The results give values ranging from slight uplift (+0.015mm/a) to subtle subsidence (−0.030 mm/a), coinciding with other author's determinations.</span></p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"706 ","pages":"Pages 60-75"},"PeriodicalIF":1.9,"publicationDate":"2024-07-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141851269","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
Paleocoastline modelling – What a difference a few meters of sediment make? 古海岸线建模--几米沉积物的差别有多大?
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-22 DOI: 10.1016/j.quaint.2024.07.005
Ana Novak
{"title":"Paleocoastline modelling – What a difference a few meters of sediment make?","authors":"Ana Novak","doi":"10.1016/j.quaint.2024.07.005","DOIUrl":"10.1016/j.quaint.2024.07.005","url":null,"abstract":"<div><p>Paleoreconstructions of coastal and near-coastal areas have always served as a tool towards better understanding of past, present and future geological and geomorphological processes. The reliability of paleocoastline and sea-land extent modelling is controlled by input data. Here the difference between paleoreconstructions based on present-day bathymetry and a paleotopographic elevation model are examined on the example of the Gulf of Trieste (northern Adriatic sea) - a low-gradient submerged Last Glacial Maximum alluvial plain with fairly well-resolved bathymetry and pre-transgressional paleotopography. Results presented in this study show striking differences between the spatial extent of the two modelled sets of paleocoastlines which in places exceeds tens of kilometers. These results demonstrate the importance of using an appropriate geologically-supported elevation model for paleoreconstruction as unsuitable models can result in significant errors and unreliable reconstructions. This is especially noteworthy for low-gradient settings where even a slight variation in sea level can affect vast areas. Finally, the results of this study provide insight into the Early Holocene evolution of the present-day area of the Gulf of Trieste as an abrupt and predominant northeasterly oriented transgression direction is indicated from the paleocoastline reconstructions.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"706 ","pages":"Pages 49-59"},"PeriodicalIF":1.9,"publicationDate":"2024-07-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S1040618224002088/pdfft?md5=109eb44274bda2c604adf5104fb291b3&pid=1-s2.0-S1040618224002088-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141838415","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
Revised OSL chronology of the Kisiljevo loess-palaeosol sequence: New insight into the dust flux in the eastern Carpathian Basin during MIS 3 - MIS1 修订的 Kisiljevo 黄土-古沉积物序列的 OSL 年表:对MIS 3 - MIS1期间喀尔巴阡山盆地东部尘埃通量的新认识
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-20 DOI: 10.1016/j.quaint.2024.06.006
Zoran M. Perić , Cathal Ryan , Helena Alexanderson , Slobodan B. Marković
{"title":"Revised OSL chronology of the Kisiljevo loess-palaeosol sequence: New insight into the dust flux in the eastern Carpathian Basin during MIS 3 - MIS1","authors":"Zoran M. Perić ,&nbsp;Cathal Ryan ,&nbsp;Helena Alexanderson ,&nbsp;Slobodan B. Marković","doi":"10.1016/j.quaint.2024.06.006","DOIUrl":"10.1016/j.quaint.2024.06.006","url":null,"abstract":"<div><p>This study presents a detailed investigation of the Kisiljevo loess-palaeosol sequence in north-eastern Serbia, offering a refined understanding of its paleoenvironmental dynamics. Contrasting our updated OSL chronology with a previous study, reveals discrepancies, particularly at 400 cm depth, where a considerable age underestimation is evident. While variations in sampling depth and methodology may contribute to some differences, the substantial deviation raises concern about the reliability of the earlier chronology. Our robust age-depth model constructed using Bayesian modelling, and the consistent increase in ages with depth suggest a potential underestimation in the uppermost layer of the earlier study, possibly due to partial bleaching or post-depositional mixing. The Bayesian age-depth model portrays a continuous sedimentation history from the later stages of Marine Isotope Stage 3 (MIS 3) to the present day. The patterns in the calculated Mass Accumulation Rates reveal distinctive peaks during MIS 3 and the middle of MIS 2, deviating from typical dust deposition models. The MIS 3 peaks in dustiness could be attributed to regional factors such as increased transportation rates, enhanced trapping efficiency, or elevated palaeowind intensity. This research not only enhances our understanding of the Kisiljevo LPS but also provides valuable insights into regional paleoenvironmental dynamics. The study emphasizes the importance of considering local geological variations in reconstructing past climates from sediment archives and sets the stage for further investigations into the factors influencing dust deposition in north-eastern Serbia. The MAR trends established here serve as a crucial reference for broader paleoclimatic interpretations in the Carpathian Basin.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"698 ","pages":"Pages 39-48"},"PeriodicalIF":1.9,"publicationDate":"2024-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S1040618224001952/pdfft?md5=603a6cc33ab3cb63b3aa72e1d771caa7&pid=1-s2.0-S1040618224001952-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141729558","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
Seismic stratigraphy of the northern area of Punta Bandera (Lago Argentino, southern Patagonia) Punta Bandera(阿根廷湖,巴塔哥尼亚南部)北部地区的地震地层学
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-20 DOI: 10.1016/j.quaint.2024.06.002
{"title":"Seismic stratigraphy of the northern area of Punta Bandera (Lago Argentino, southern Patagonia)","authors":"","doi":"10.1016/j.quaint.2024.06.002","DOIUrl":"10.1016/j.quaint.2024.06.002","url":null,"abstract":"<div><p>Lago Argentino is one of the largest lakes in Patagonia. Some of its arms host calving glaciers that flow from the southern Patagonian Ice Field. The best known of these is the Perito Moreno glacier. Although recent studies have reconstructed part of glacier dynamics in the southern arms of Lago Argentino, there are no studies yet for the northern arms. A high-resolution seismic survey was carried out in the northern area of Punta Bandera, i.e., in the sector between the Brazo Norte and the Canal de los Témpanos to characterize the stratigraphy of the sedimentary fill of the lake and identify the main unconformities related to glacial dynamics. Eight seismic facies grouped into two seismic units were mapped, and ten unconformities were recognized. Based on the acquired data, a bathymetric grid was created for the first time to obtain a morphological representation of the lake floor and access to a previously unmapped area of Lago Argentino. The analysis of the geometries and acoustic properties of the different seismic facies identified, correlated with the available information on land moraines, has allowed us to partially reconstruct the advance and retreat phases of the glacial lobes that formerly were present in the two arms of the lake, although the temporal assignments are still speculative due to the lack of calibrations with boreholes. Nevertheless, this study provides important information for deciphering the glaciation history of a key sector of the southern Patagonian Ice Field during the late Pleistocene/Holocene. The data show that the northern and southern areas have different lake floor morphologies, with the southern, shallower area of the Canal de los Témpanos being glaciated first than the northern, more overdeepened area of the Brazo Norte.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"698 ","pages":"Pages 26-38"},"PeriodicalIF":1.9,"publicationDate":"2024-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141392587","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
Chronology of late Holocene sediments related to the Qicheng ruins in central China 与中国中部启城遗址有关的全新世晚期沉积物的年代学研究
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-20 DOI: 10.1016/j.quaint.2024.05.005
{"title":"Chronology of late Holocene sediments related to the Qicheng ruins in central China","authors":"","doi":"10.1016/j.quaint.2024.05.005","DOIUrl":"10.1016/j.quaint.2024.05.005","url":null,"abstract":"<div><p>The Qicheng city wall is located in Puyang, Henan Province, China, and it is an important archaeological site from the Neolithic period in the North China Plain region. A trench across the northwest corner of the city wall revealed an 11 m thick sediment sequence, closely associated with human activities, which provides valuable records for the dating and environmental evolution of the site. In this study, we have applied field geological investigation, grain size analysis, optically stimulated luminescence (OSL) dating, and radiocarbon (<sup>14</sup>C) dating to reveal the history and changes in the site. The ancient city wall was built on the sedimentary sequence (U1) of the high terrace of the Ancient Yellow River. The upper 11 m thick sedimentary sequence (U2) recorded early moat sedimentation (U2<sub>L</sub>) and was followed by three cycles of paleosol-flooding deposits (U2<sub>U</sub>). The quartz OSL signals of the U2 silts are extremely bright, indicating high sensitivity. Partial bleaching was observed as well. The quartz OSL single-grain SAR dating results are consistent with that of charcoal <sup>14</sup>C dating and are closer to the ‘true’ burial ages of the sediments than those obtained with multiple grains. By using a Bayesian statistical model, a chronological framework for the U2 sedimentary sequence was established. The earliest construction date of the Qicheng city wall is dating to 2100–1300 BC, during the late Longshan period, which is consistent with archaeological evidence (Li et al., 2015). The Qicheng city was not significantly affected by paleo-flooding prior to 870–960 AD, but experiences frequent flooding thereafter.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"698 ","pages":"Pages 1-10"},"PeriodicalIF":1.9,"publicationDate":"2024-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141501170","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
Influence of Na-feldspar grains within the K-feldspar fraction on sediments IRSL dating K长石部分中的钠长石颗粒对沉积物IRSL年代测定的影响
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-20 DOI: 10.1016/j.quaint.2024.06.009
Dongxue Li , Hui Zhao , Haichao Xie , Farhad Khormali , Aijun Sun , Shuai Zhang
{"title":"Influence of Na-feldspar grains within the K-feldspar fraction on sediments IRSL dating","authors":"Dongxue Li ,&nbsp;Hui Zhao ,&nbsp;Haichao Xie ,&nbsp;Farhad Khormali ,&nbsp;Aijun Sun ,&nbsp;Shuai Zhang","doi":"10.1016/j.quaint.2024.06.009","DOIUrl":"10.1016/j.quaint.2024.06.009","url":null,"abstract":"<div><p>The post-Infrared Infrared Stimulated Luminescence (pIRIR) protocol has been successfully applied to date Quaternary sediments using the K-rich feldspar fraction (density <2.58 g/cm<sup>3</sup>). However, during the extraction of K-feldspar grains, Na-feldspar particles (density 2.58–2.62 g/cm<sup>3</sup>) may be included, especially within the medium grained fraction. However, the possible influence of Na-feldspar contamination on K-feldspar IRSL dating results has not been investigated in detail. In this study, we applied the pIRIR dating protocol to measure the coarse- and medium-grained K-and Na-feldspar fractions of eight aeolian samples from various regions. Blue-violet and yellow-green detection windows were used for derived the signals of K- and Na-feldspar, respectively, and we attempted to evaluate the influence of the contamination by Na-feldspar grains on feldspar pIRIR dating. Comparison of the three signals (K-feldspar blue, Na-feldspar blue, Na-feldspar yellow) from each sample showed that the influence of the IRSL blue signal from Na-feldspar grains on the signal of the K-feldspar fraction was &lt; 1–3%. Because of high fading rates, the D<sub>e</sub>s or pIRIR ages obtained from the Na-feldspar yellow signal were underestimated. The Na-feldspar blue pIRIR D<sub>e</sub>s and ages were nevertheless consistent with their corresponding K-feldspar blue D<sub>e</sub> values and ages. This is because the few K-feldspar grains included within the Na-feldspar fraction emitted the greater part of the blue signals. From these observations, we conclude that the influence of Na-feldspar grains within the K-feldspar fraction on K-feldspar IRSL dating results can be ignored.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"698 ","pages":"Pages 49-58"},"PeriodicalIF":1.9,"publicationDate":"2024-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141729557","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
California Current temperatures adjacent to Southern California: 1949–2020 南加州附近的加州洋流温度:1949-2020 年
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-20 DOI: 10.1016/j.quaint.2024.07.004
Steve Lund
{"title":"California Current temperatures adjacent to Southern California: 1949–2020","authors":"Steve Lund","doi":"10.1016/j.quaint.2024.07.004","DOIUrl":"10.1016/j.quaint.2024.07.004","url":null,"abstract":"<div><p><span><span>The southward flowing California Current, which lies adjacent to the California Pacific coastline as part of the North Pacific Ocean gyre circulation, is an important element in characterizing California's </span>climate variability<span>. This study improves and extends the historic record of California Current temperatures along the Southern California coastline for the last 71 years. The data come from long-term sea surface temperature measurements determined by the California Cooperative Oceanic Fisheries Investigations (CalCOFI) partners. The sea-surface temperature measurements come from a grid of 31 oceanic sampling sites within the core of the California Current off the Southern California coast. The sites have been sampled intermittently over the course of each year with ∼100 measurements/year on average. The Southern California Current temperatures in our grid have risen ∼2.5 °C since 1949.The California current temperatures are strongly correlated with the larger-scale North Pacific Ocean </span></span>Pacific Decadal Oscillation<span> (PDO) index and the North Pacific Gyre Oscillation (NGPO) index. All three show distinctive correlation with decadal (∼14-yr) California rainfall cyclicity.</span></p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"705 ","pages":"Pages 104-108"},"PeriodicalIF":1.9,"publicationDate":"2024-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141846585","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
Tsunami deposits in tropical regions: A review 热带地区的海啸沉积物:综述
IF 1.9 3区 地球科学
Quaternary International Pub Date : 2024-07-20 DOI: 10.1016/j.quaint.2024.06.001
{"title":"Tsunami deposits in tropical regions: A review","authors":"","doi":"10.1016/j.quaint.2024.06.001","DOIUrl":"10.1016/j.quaint.2024.06.001","url":null,"abstract":"<div><p>Tsunami deposits provide evidence of historical and prehistorical events. However, their preservation in tropical regions is generally poor. The reasons behind this poor preservation are often linked to a number of environmental and anthropogenic factors. This study is focused on analyzing the environmental factors that impact the preservation and availability of tsunami deposits specifically in tropical regions. These factors predominantly encompass climate-related elements such as consistently high temperatures, rainfall, humidity, as well as specific soil processes, oceanic conditions, and vegetation. We compiled a comprehensive database of scientific publications on tsunami deposits, identifying the geomorphic environments where such deposits are typically preserved, as well as the commonly utilized proxies in studying tsunami deposits across different climatic zones. We propose a model that outlines the environmental factors, processes, and their interrelationships that contribute to the preservation and availability of tsunami deposits in tropical regions. This model may prove valuable in the future identification of tsunami deposits in tropical areas.</p></div>","PeriodicalId":49644,"journal":{"name":"Quaternary International","volume":"698 ","pages":"Pages 11-25"},"PeriodicalIF":1.9,"publicationDate":"2024-07-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S1040618224001836/pdfft?md5=1906bfe45738d953af4d7ff913621402&pid=1-s2.0-S1040618224001836-main.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141396115","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
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