Holocene最新文献_第4页

Isolation basin stratigraphy and Holocene relative sea-level change on the Barents Sea coast at Teriberka, Kola Peninsula, northwestern Russia 俄罗斯西北部科拉半岛捷利别尔卡巴伦支海岸隔离盆地地层与全新世相对海平面变化

IF 2.4 3区地球科学

Holocene Pub Date : 2023-05-28 DOI: 10.1177/09596836231176489

V. Kolka, D. Tolstobrov, G. D. Corner, O. Korsakova, Alena Tolstobrova, A. Vashkov

{"title":"Isolation basin stratigraphy and Holocene relative sea-level change on the Barents Sea coast at Teriberka, Kola Peninsula, northwestern Russia","authors":"V. Kolka, D. Tolstobrov, G. D. Corner, O. Korsakova, Alena Tolstobrova, A. Vashkov","doi":"10.1177/09596836231176489","DOIUrl":"https://doi.org/10.1177/09596836231176489","url":null,"abstract":"The paper presents isolation basin stratigraphy in bottom sediments from nine lakes in the Teriberka area on the Kola Peninsula, northwestern Russia. Isolation contacts in these basins, identified from lithological and diatom analysis, were used together with 25 radiocarbon dates, to construct a relative sea-level (RSL) curve for the Holocene. Records of marine water re-influx were found in the sediment sequence from one lake, located at c. 17 m a.s.l. The re-influx of marine water seems to be caused by the mid-Holocene (Tapes) transgression and tsunami event. The RSL curve indicates several phases in the postglacial evolution of the Kola coast. An early phase of rapid sea-level fall of c. 32 m around 11,500 cal yr BP, at a rate of c. 40 mm per year, corresponds to glacio-isostatically induced emergence following deglaciation at the Younger Dryas and beginning of the Holocene. In the time interval between c. 11,000 and 7600 cal yr BP, either a stillstand or a slight rise in relative sea level, cresting at about 21 m a.s.l., is suggested in the Teriberka area. This is followed, after c. 7300 cal yr BP to the present day, by a slow glacioisostatic emergence with an average rate of about 2–3 mm per year.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"1060 - 1072"},"PeriodicalIF":2.4,"publicationDate":"2023-05-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44145423","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

Youngest Iberian Holocene volcanic eruptions and paleoenvironmental evolution of a barrier-paleolake in the Garrotxa Volcanic Field (NE Spain) 西班牙东北部Garrotxa火山场最年轻伊比利亚全新世火山喷发与障壁古湖泊古环境演化

IF 2.4 3区地球科学

Holocene Pub Date : 2023-05-17 DOI: 10.1177/09596836231169989

E. Iriarte, J. Revelles, W. Finsinger, F. Mesquita‐Joanes, M. A. Rodrigo, F. Burjachs, I. Expósito, J. Martí Molist, L. Planagumà, G. Alcalde, M. Saña

{"title":"Youngest Iberian Holocene volcanic eruptions and paleoenvironmental evolution of a barrier-paleolake in the Garrotxa Volcanic Field (NE Spain)","authors":"E. Iriarte, J. Revelles, W. Finsinger, F. Mesquita‐Joanes, M. A. Rodrigo, F. Burjachs, I. Expósito, J. Martí Molist, L. Planagumà, G. Alcalde, M. Saña","doi":"10.1177/09596836231169989","DOIUrl":"https://doi.org/10.1177/09596836231169989","url":null,"abstract":"Volcanic eruptions are key drivers of climate variability, with complex environmental consequences at regional and local scales that are rarely documented in high-resolution sedimentary records. In this work we present the results of a 15 m long paleolake core (Pla de les Preses core, Vall d’en Bas, Girona, NE Spain) covering the Late Pleistocene-Holocene transition. Multiproxy analyses including chronostratigraphy, sedimentology, micropalaeontology and geochemistry are used to reconstruct the paleoenvironmental framework of the Late Pleistocene-Holocene transition and to detect the youngest Holocene volcanic eruptions in the Garrotxa Volcanic Field (GVF) and the Iberian Peninsula. The studied sedimentary record covers the last ca. 13.5 ka cal BP and was punctuated by several rapid climatic changes including the 9.3, 8.2 and 7.1 ka events, affecting the hydrological evolution of a barrier-lake formed due to the volcanic damming of the Fluvià river. Sedimentological and geochemical analyses unveil the environmental history of Vall d’en Bas valley; the formation of a lacustrine area within a fluvial environment around 13.5 ka cal BP and later a wetland phase between 9.3 and 8.2 ka cal BP. Abrupt sedimentary changes marking the onset and demise of the wetland phase were linked to hemispheric cooling and drying events (e.g. 9.3 and 8.2 ka cal BP), provoking a decline in the water table during these phases. In addition, 30 tephra layers are detected thorough the core, showing previously unknown intense volcanic activity from 13.5 to 8.3 ka cal BP in the GVF. In that sense, the Pla de les Preses sequence provides, for the first time, evidence for early Holocene volcanic activity in NE Iberia that should be taken into account in future tephra studies in the western Mediterranean realm.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"939 - 959"},"PeriodicalIF":2.4,"publicationDate":"2023-05-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43023437","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: 1

Different hydrological controls causing variable rates of Holocene peat growth in a lowland valley system, north-eastern Netherlands; implications for valley peatland restoration 不同水文控制导致荷兰东北部低地河谷系统全新世泥炭生长速率的变化对河谷泥炭地恢复的启示

IF 2.4 3区地球科学

Holocene Pub Date : 2023-05-11 DOI: 10.1177/09596836231169985

B. Makaske, G. J. Maas

{"title":"Different hydrological controls causing variable rates of Holocene peat growth in a lowland valley system, north-eastern Netherlands; implications for valley peatland restoration","authors":"B. Makaske, G. J. Maas","doi":"10.1177/09596836231169985","DOIUrl":"https://doi.org/10.1177/09596836231169985","url":null,"abstract":"The Drentsche Aa valley system in the glacial sandy landscape of the north-eastern Netherlands, is one of the many regional drainage systems in the north-western to central European Lowlands. Following deep incision in the Weichselian, ca 7 m of eutrophic peat has accumulated in the lower to middle reaches of the valley system in the Holocene, completely filling the Weichselian incision. We reconstructed the rate of water-level rise controlling peat growth at three locations in the valley system (representing the upper, middle and lower reaches), using 14C peat dates from compaction-free sampling sites on the sloping valley margin where the peat directly overlies the sandy Pleistocene subsurface. The 14C dates enabled the construction of curves showing the water-level evolution at each location. Our results show variable rates of Holocene peat growth in the valley system in response to different drivers of hydrological change: a strong increase in annual precipitation (onset Holocene), a decrease in evapotranspiration (10,000–8000 cal. years BP) and relative sea-level rise (after ~4500 cal. years BP). Because the identified hydrological controls on peat growth are regional, they probably ruled Holocene peat growth in many peat-filled valley systems in the north-western to central European Lowlands. Currently, there is growing attention for these valley systems in the context of European nature restoration efforts and climate change adaptation and mitigation measures. The present study underscores that large-scale hydrological measures outside the valley system are needed for restoration of degraded valley peatlands.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"960 - 974"},"PeriodicalIF":2.4,"publicationDate":"2023-05-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42428182","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

Early afforestation on islands of proglacial Lake Ojibway as evidence of post-glacial migration outposts 前冰期奥吉布威湖岛屿上的早期造林作为冰期后移民前哨的证据

IF 2.4 3区地球科学

Holocene Pub Date : 2023-05-10 DOI: 10.1177/09596836231169988

M. Vogel, Hugo Asselin, S. Joannin, Y. Bergeron, Sabrina Leclercq, Cécile Latapy, Adam A. Ali

{"title":"Early afforestation on islands of proglacial Lake Ojibway as evidence of post-glacial migration outposts","authors":"M. Vogel, Hugo Asselin, S. Joannin, Y. Bergeron, Sabrina Leclercq, Cécile Latapy, Adam A. Ali","doi":"10.1177/09596836231169988","DOIUrl":"https://doi.org/10.1177/09596836231169988","url":null,"abstract":"At the end of the last glacial period in the northern hemisphere, meltwater from receding ice sheets accumulated into large proglacial lakes, potentially limiting postglacial afforestation. We explored whether former islands of proglacial Lake Ojibway (Canada) (hilltops in the current landscape) could have acted as migration outposts and thus accelerated the postglacial migration. We extracted sediments from two small lakes located on “paleo-islands” and used XRF to detect changes in soil erosion and vegetation biomass. We also used plant macro-remains and wood charcoal to determine if (and which) tree species colonized the sites and to detect local fire events. Organic sediment accumulation started around 9657 and 9947 cal. yr BP at Lakes Perché and Despériers, respectively, before the level of Lake Ojibway started to decrease and liberate parts of the studied landscape ca 9400 cal. yr BP. Lithogenic elements (Ti, K, Sr, Fe, Zr, and Rb) decreased between the beginning of organic sediment accumulation and 8800–8700 cal. yr BP, indicating reduced soil erosion, possibly due to soil stabilization by vegetation. Then, the S/Ti ratio, a proxy of organic matter increased around 8800 and 8400 cal. yr BP. The earliest tree macro-remains (Larix laricina and Pinus spp.) were found between 9850 and 9500 cal. yr BP. Local fires were detected around 9820 and 8362 cal. yr BP. Early afforestation occurred on the islands of Lake Ojibway, 200 and 450 years before its level started to decrease, confirming that some islands acted as migratory outposts accelerating postglacial migration.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"975 - 985"},"PeriodicalIF":2.4,"publicationDate":"2023-05-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44376943","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

IF 2.4 3区地球科学

Holocene Pub Date : 2023-05-08 DOI: 10.1177/09596836221145418

Peizheng He, Xingqi Liu, H. Sun, Shengnan Feng, Xin Mao

{"title":"ENSO-related centennial and millennial-scale hydroclimate changes recorded from Lake Xiaolongchi in arid Central Asia over the past 8000 years","authors":"Peizheng He, Xingqi Liu, H. Sun, Shengnan Feng, Xin Mao","doi":"10.1177/09596836221145418","DOIUrl":"https://doi.org/10.1177/09596836221145418","url":null,"abstract":"Climate changes on different timescales and their mechanisms are of great importance in arid Central Asia (ACA). However, the contribution of El Niño−Southern Oscillation (ENSO) to Holocene hydroclimate in ACA on centennial and millennial timescales is limited by records with good age control and high temporal resolution. Here, we present high-resolution X-ray fluorescence (XRF) scanning data of a sediment core from Lake Xiaolongchi in central Tianshan Mountains to reconstruct hydroclimate changes in ACA over the last 8000 years. Our construction exhibits that the climate was dry from 8000 to 5500 cal year BP and wet from 5500 to 0 cal year BP, which resembles ENSO patterns on a millennial timescale. On the centennial timescale, hydroclimate fluctuations with eight wet periods, seven dry periods, and a shift period have a significant 800-year periodicity, coincident with periodic ENSO variance. The positive relationship between 800-year band-pass filtered hydroclimate and ENSO indicates that wet (dry) climate conditions correspond to increased (reduced) ENSO activity. We propose that the spatial pattern of “wet (dry) southern China and ACA, and dry (wet) northern China” during the El Niño-like (La Niña-like) condition may exist during the Holocene on millennial to centennial timescales.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"880 - 889"},"PeriodicalIF":2.4,"publicationDate":"2023-05-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43311184","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

A guide to assess distance from ecological baselines and change over time in palaeoecological records 评估古生态记录中与生态基线的距离和随时间变化的指南

IF 2.4 3区地球科学

Holocene Pub Date : 2023-04-29 DOI: 10.1177/09596836231169986

O. Burge, S. Richardson, Jamie R. Wood, J. Wilmshurst

{"title":"A guide to assess distance from ecological baselines and change over time in palaeoecological records","authors":"O. Burge, S. Richardson, Jamie R. Wood, J. Wilmshurst","doi":"10.1177/09596836231169986","DOIUrl":"https://doi.org/10.1177/09596836231169986","url":null,"abstract":"Palaeoecology provides critical data for establishing ecological ‘baselines’, which can guide restoration efforts and be used to assess ecosystem change. However, statistical analyses can be challenging because of the large number of methods available for establishing palaeoecological baselines combined with a lack of practical guidance, particularly around quantifying baselines that include natural variability. We contribute one solution by providing guidance and an R package baselines for using palaeoecological data to (i) define baselines and (ii) test for change over time that incorporates variability. These methods provide an alternative to single-taxon analyses and allow ecosystem complexity to be captured. We use published pollen records as case studies to demonstrate how to establish vegetation baselines for seven localities in New Zealand where relatively recent (c. 1280 AD) and near-simultaneous human settlement across the country allows background environmental disturbance in the pre-human era to be distinguished from anthropogenic disturbance. We present methods for calculating distance from initial sample, distance from baseline in ordination space, allowing incorporation of ecosystem variability, and analysis of rates of change over time using principal curves. We found conventional and Bayesian ordination methods yielded similar results and were effective at identifying change following human settlement, despite the potential for a positive mean-variance relationship to confound results. Principal response curves were most sensitive to a known period of vegetation disturbance caused by volcanic eruptions at two sites with tephra deposits. Our proposed methods, case study and R package baselines are designed to provide a suite of tools to encourage and enable palaeoecological data to be used by palaeoecologists to assess trajectories and change over time, and monitor whether historical management actions have facilitated a change in direction towards a desired baseline state.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"905 - 917"},"PeriodicalIF":2.4,"publicationDate":"2023-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44379165","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: 1

Holocene relative sea-level changes in northwest Ireland: An empirical test for glacial isostatic adjustment models 爱尔兰西北部全新世相对海平面变化：冰川均衡调整模型的经验检验

IF 2.4 3区地球科学

Holocene Pub Date : 2023-04-29 DOI: 10.1177/09596836231169992

J. Kirby, E. Garrett, W. Gehrels

{"title":"Holocene relative sea-level changes in northwest Ireland: An empirical test for glacial isostatic adjustment models","authors":"J. Kirby, E. Garrett, W. Gehrels","doi":"10.1177/09596836231169992","DOIUrl":"https://doi.org/10.1177/09596836231169992","url":null,"abstract":"The late-Quaternary relative sea-level (RSL) history of Ireland is complex, positioned at the margins of the former British-Irish Ice Sheet, and subject to the influence of ice unloading and forebulge collapse. Geophysical models of post-glacial isostatic adjustment (GIA) provide estimates of the pattern of RSL change since deglaciation which may be tested and validated with empirical data from proxy records. For the region of northwest Ireland, there is a paucity of high-quality RSL data and, therefore, equivocal evidence to support the GIA models that predict a mid to Late-Holocene RSL highstand of between +0.5 and +2 m above present. This study aims to investigate this model-data discrepancy by reconstructing RSL change from a near continuous salt-marsh sequence at Bracky Bridge, Donegal, spanning the last ca. 2500 years. We develop a transfer function model to reconstruct the vertical position of sea level using a regional diatom training set to quantify the indicative meaning and predict the palaeomarsh elevation of the core samples. A chronology is provided by a combination of 14C and 210Pb data, with sample specific ages derived from an age-depth model using a Bayesian framework. Our reconstruction shows ca. 2 m of relative sea-level rise in the past 2500 years. This is not compatible with some previously published sea-level index points from the region, which we re-interpret as freshwater/terrestrial limiting data. These results do not provide any evidence to support a Mid-Holocene RSL highstand above present sea level. Whilst none of the available GIA models replicate the timing and magnitude of the Late-Holocene RSL rise in our reconstruction, those which incorporate a thick and extensive British-Irish Sea Ice Sheet provide the best fit.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"926 - 938"},"PeriodicalIF":2.4,"publicationDate":"2023-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43645980","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: 2

An 11,000 year record of plant community stability and paludification in a patterned rich fen in northeastern Alberta, Canada 加拿大艾伯塔省东北部一个模式丰富的沼泽地植物群落稳定性和沼泽化的11000年记录

IF 2.4 3区地球科学

Holocene Pub Date : 2023-04-25 DOI: 10.1177/09596836231169997

D. Vitt, Melissa House

{"title":"An 11,000 year record of plant community stability and paludification in a patterned rich fen in northeastern Alberta, Canada","authors":"D. Vitt, Melissa House","doi":"10.1177/09596836231169997","DOIUrl":"https://doi.org/10.1177/09596836231169997","url":null,"abstract":"Patterned rich fens have a diverse flora and are maintained by unidirectional inflowing water with high concentrations of base cations, along with high pH and limited nutrients. Rich fens are among the most threatened ecosystems in Europe, but are not uncommon across the western boreal forest zone of Canada. Utilizing 10 radiocarbon dated cores extracted from the wetland, we investigated the Holocene developmental history of a large patterned rich fen in northeastern Alberta (McClelland Wetland). Organic matter accumulation began around 11,457 cal yr BP as primary peat formation on recently deglaciated substrates. Over the 10,000+ years history of McClelland Wetland, the central portions of the wetland have been remarkably resistant to change, with little alteration in dominant species. The resistance to change is set against a background of fluctuations in regional Holocene climate and local varying water balance. The dominant bryophyte species (Hamatocaulis vernicosus and Scorpidium scorpioides) continued to play a foundational role on site for the duration of the Holocene, dependent on a persistent long-term ground water source. Accumulation rates of organic matter have remained steady once the dominant bryophyte layer was established, but with accumulation rates at paludifying marginal sites lower than those of the central moss-graminoid-dominated areas.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"33 1","pages":"986 - 997"},"PeriodicalIF":2.4,"publicationDate":"2023-04-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47422944","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

Comparison of the Polyamine Content of Five Spring Flowers with Wheat Germ as a Rich Anti-aging Polyamine Source for Preparation of Nutraceutical Products. 比较五种春花与小麦胚芽中的多胺含量，为制备营养保健品提供丰富的抗衰老多胺来源

IF 1.6 3区地球科学

Holocene Pub Date : 2023-04-25 eCollection Date: 2023-01-01 DOI: 10.5812/ijpr-134938

Maryam Mohajeri, Seyed Abdulmajid Ayatollahi, Mohammad Goli, Shaya Mokhtari, Maryam Khandan, Azadeh Nasiri, Farzad Kobarfard

{"title":"Comparison of the Polyamine Content of Five Spring Flowers with Wheat Germ as a Rich Anti-aging Polyamine Source for Preparation of Nutraceutical Products.","authors":"Maryam Mohajeri, Seyed Abdulmajid Ayatollahi, Mohammad Goli, Shaya Mokhtari, Maryam Khandan, Azadeh Nasiri, Farzad Kobarfard","doi":"10.5812/ijpr-134938","DOIUrl":"10.5812/ijpr-134938","url":null,"abstract":"Polyamines prolong longevity due to their role in cell proliferation and are regarded as an essential group of anti-aging substances that reduce the risk of cardiovascular, neurological, and chronic inflammatory illnesses, as well as cancer. Because of its importance in growth and tissue regeneration, discovering polyamine-rich sources has gotten a lot of interest. Given the role of polyamines in controlling plant growth and physiological changes in the spring after cold winter stress, high polyamine concentrations in quickly growing plant tissues such as flowers, blossoms, and germs are possible. Based on this premise, five different spring flowers were selected and isolated from relevant plants, dried, and then quantified for the first time using an accurate, simple, and repeatable quantification method, liquid chromatography-tandem mass spectrometry. According to the amount of spermidine found in the samples investigated in this study, dried flower powders of Wisteria sinensis (244.18 µg/g), Lonicera caprifolium (217.28 µg/g), and Jasminum officinale (200.33 µg/g) appear to be a good source of spermidine. With additional research, W. sinensis dried flower powder is a good source of polyamines, whereas L. caprifolium and J. officinale dried flower powders are recommended as a rich source of spermidine for the preparation of natural supplements for people over the age of 30 to improve cell proliferation and anti-aging.","PeriodicalId":50402,"journal":{"name":"Holocene","volume":"6 1","pages":"e134938"},"PeriodicalIF":1.6,"publicationDate":"2023-04-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10728854/pdf/","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"87265340","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

Preboreal oscillation in the light of multiproxy analyses—Early Holocene in Lake Jelonek (North Poland) 多代用物分析下的波兰北部耶洛内克湖早全新世前寒带振荡

IF 2.4 3区地球科学

Holocene Pub Date : 2023-04-25 DOI: 10.1177/09596836231169993

M. Kramkowski, Anna Filbrand-Czaja, E. Zawisza, M. Rzodkiewicz, B. Kotrys, J. Mirosław‐Grabowska, M. Błaszkiewicz, Krzysztof Szewczyk, M. Słowiński

引用次数: 0