• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利：CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法，用中文像聊天一样搜索，搜遍4000万医学文献。AI智能推荐，让科研检索更轻松。

立即免费搜索

文件翻译

保留排版，准确专业，支持PDF/Word/PPT等文件格式，支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述，25分钟生成高质量综述，智能提取关键信息，辅助科研写作。

立即免费体验

多瑙河下游的尼安德特人：巴尔干半岛多瑙河峡谷的旧石器时代中期证据。

Neanderthals on the Lower Danube: Middle Palaeolithic evidence in the Danube Gorges of the Balkans.

作者信息

Borić Dušan, Cristiani Emanuela, Hopkins Rachel, Schwenninger Jean-Luc, Gerometta Katarina, French Charly A I, Mutri Giuseppina, Ćalić Jelena, Dimitrijević Vesna, Marín-Arroyo Ana B, Jones Jennifer R, Stevens Rhiannon, Masciana Alana, Uno Kevin, Richter Kristine Korzow, Antonović Dragana, Wehr Karol, Lane Christine, White Dustin

机构信息

The Italian Academy for Advanced Studies in America Columbia University New York NY USA.

Department of Environmental Biology Sapienza University of Rome Rome Italy.

出版信息

J Quat Sci. 2022 Feb;37(2):142-180. doi: 10.1002/jqs.3354. Epub 2021 Aug 25.

DOI:10.1002/jqs.3354
PMID:35874300
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9291232/
Abstract

The article presents evidence about the Middle Palaeolithic and Middle to Upper Palaeolithic transition interval in the karst area of the Danube Gorges in the Lower Danube Basin. We review the extant data and present new evidence from two recently investigated sites found on the Serbian side of the Danube River - Tabula Traiana and Dubočka-Kozja caves. The two sites have yielded layers dating to both the Middle and Upper Palaeolithic and have been investigated by the application of modern standards of excavation and recovery along with a suite of state-of-the-art analytical procedures. The presentation focuses on micromorphological analyses of the caves' sediments, characterisation of cryptotephra, a suite of new radiometric dates (accelerator mass spectrometry and optically stimulated luminescence) as well as proteomics (zooarchaeology by mass spectrometry) and stable isotope data in discerning patterns of human occupation of these locales over the long term.

摘要

本文展示了多瑙河下游盆地多瑙河峡谷岩溶地区中旧石器时代和中旧石器时代向旧石器时代晚期过渡阶段的相关证据。我们回顾了现有数据，并展示了来自多瑙河塞尔维亚一侧最近调查的两个遗址——图拉真石板和杜博奇卡-科贾洞穴的新证据。这两个遗址都有可追溯到中旧石器时代和旧石器时代晚期的地层，并且已按照现代发掘和回收标准以及一系列最先进的分析程序进行了调查。报告重点关注洞穴沉积物的微形态分析、隐伏火山灰的特征描述、一系列新的放射性测年数据（加速器质谱法和光释光法）以及蛋白质组学（质谱动物考古学）和稳定同位素数据，以识别这些地区长期人类居住的模式。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/ad5dcbcb2f2c/JQS-37-142-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/0469edc2299a/JQS-37-142-g018.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/9a9045f2c639/JQS-37-142-g013.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/f3870fde87c8/JQS-37-142-g017.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/7fa025f3df10/JQS-37-142-g024.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/6925bb5f48ae/JQS-37-142-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/2dacc24e926b/JQS-37-142-g011.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/a52985f18607/JQS-37-142-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/be351e6f6072/JQS-37-142-g020.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/bc89af409535/JQS-37-142-g023.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/f44d419cd42e/JQS-37-142-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/64fb6780f25a/JQS-37-142-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/0782714c4664/JQS-37-142-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/e0b5d9117003/JQS-37-142-g010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/fee0d7d2815d/JQS-37-142-g019.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/f600b95da0a2/JQS-37-142-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/de998d5ab46a/JQS-37-142-g016.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/67c933a29211/JQS-37-142-g012.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/371410d5cf54/JQS-37-142-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/5bd1655d5188/JQS-37-142-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/8c56d7d33774/JQS-37-142-g015.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/6d333dc59ab8/JQS-37-142-g014.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/ced5f727bdac/JQS-37-142-g021.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/25bc15845869/JQS-37-142-g022.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/ad5dcbcb2f2c/JQS-37-142-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/0469edc2299a/JQS-37-142-g018.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/9a9045f2c639/JQS-37-142-g013.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/f3870fde87c8/JQS-37-142-g017.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/7fa025f3df10/JQS-37-142-g024.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/6925bb5f48ae/JQS-37-142-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/2dacc24e926b/JQS-37-142-g011.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/a52985f18607/JQS-37-142-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/be351e6f6072/JQS-37-142-g020.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/bc89af409535/JQS-37-142-g023.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/f44d419cd42e/JQS-37-142-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/64fb6780f25a/JQS-37-142-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/0782714c4664/JQS-37-142-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/e0b5d9117003/JQS-37-142-g010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/fee0d7d2815d/JQS-37-142-g019.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/f600b95da0a2/JQS-37-142-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/de998d5ab46a/JQS-37-142-g016.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/67c933a29211/JQS-37-142-g012.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/371410d5cf54/JQS-37-142-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/5bd1655d5188/JQS-37-142-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/8c56d7d33774/JQS-37-142-g015.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/6d333dc59ab8/JQS-37-142-g014.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/ced5f727bdac/JQS-37-142-g021.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/25bc15845869/JQS-37-142-g022.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df3f/9291232/ad5dcbcb2f2c/JQS-37-142-g007.jpg

相似文献

1
Neanderthals on the Lower Danube: Middle Palaeolithic evidence in the Danube Gorges of the Balkans.多瑙河下游的尼安德特人：巴尔干半岛多瑙河峡谷的旧石器时代中期证据。
J Quat Sci. 2022 Feb;37(2):142-180. doi: 10.1002/jqs.3354. Epub 2021 Aug 25.
2
Revisiting the Middle and Upper Palaeolithic archaeology of Gruta do Caldeirão (Tomar, Portugal).重新审视葡萄牙托马尔卡尔德龙洞穴（Gruta do Caldeirão）的中石器时代和旧石器时代晚期考古学。
PLoS One. 2021 Oct 27;16(10):e0259089. doi: 10.1371/journal.pone.0259089. eCollection 2021.
3
New evidence of early Neanderthal disappearance in the Iberian Peninsula.伊比利亚半岛尼安德特人早期消失的新证据。
J Hum Evol. 2014 Oct;75:16-27. doi: 10.1016/j.jhevol.2014.06.002. Epub 2014 Jul 10.
4
Large-scale application of palaeoproteomics (Zooarchaeology by Mass Spectrometry; ZooMS) in two Palaeolithic faunal assemblages from China.在中国两个旧石器时代动物群中大规模应用古蛋白组学（质谱法的动物考古学；ZooMS）。
Proc Biol Sci. 2023 Oct 25;290(2009):20231129. doi: 10.1098/rspb.2023.1129.
5
New electron spin resonance (ESR) ages from Geißenklösterle Cave: A chronological study of the Middle and early Upper Paleolithic layers.盖森克勒特洞穴的新电子自旋共振（ESR）年代：中石器时代和早期旧石器时代晚期的年代学研究。
J Hum Evol. 2019 Aug;133:133-145. doi: 10.1016/j.jhevol.2019.05.014. Epub 2019 Jul 1.
6
A C chronology for the Middle to Upper Palaeolithic transition at Bacho Kiro Cave, Bulgaria.保加利亚 Bacho Kiro 洞穴中、上旧石器时代过渡期的 C 年代测定。
Nat Ecol Evol. 2020 Jun;4(6):794-801. doi: 10.1038/s41559-020-1136-3. Epub 2020 May 11.
7
The chronostratigraphy of the Haua Fteah cave (Cyrenaica, northeast Libya).哈瓦法提洞穴（利比亚东北部昔兰尼加）的年代地层学。
J Hum Evol. 2014 Jan;66:39-63. doi: 10.1016/j.jhevol.2013.10.001. Epub 2013 Dec 12.
8
Stratigraphic and technological evidence from the Middle Palaeolithic-Châtelperronian-Aurignacian record at the Bordes-Fitte rockshelter (Roches d'Abilly site, Central France).法国中部罗什迪比利遗址博尔德-菲特岩石掩蔽所（Bordes-Fitte rockshelter）中中更新世旧石器时代中期-夏特佩伦文化-奥瑞纳文化时期的地层和技术证据。
J Hum Evol. 2012 Jan;62(1):116-37. doi: 10.1016/j.jhevol.2011.10.009. Epub 2011 Dec 10.
9
New chronology for the Middle Palaeolithic of the southern Caucasus suggests early demise of Neanderthals in this region.南高加索中更新世的新年代学表明，尼安德特人在该地区的早期灭绝。
J Hum Evol. 2012 Dec;63(6):770-80. doi: 10.1016/j.jhevol.2012.08.004. Epub 2012 Oct 18.
10
Pre-Solutrean rock art in southernmost Europe: Evidence from Las Ventanas Cave (Andalusia, Spain).欧洲最南端的前索尔图雷岩画：来自拉斯文塔纳斯洞穴（西班牙安达卢西亚）的证据。
PLoS One. 2018 Oct 17;13(10):e0204651. doi: 10.1371/journal.pone.0204651. eCollection 2018.

引用本文的文献

1
Aurignacian dynamics in Southeastern Europe based on spatial analysis, sediment geochemistry, raw materials, lithic analysis, and use-wear from Românești-Dumbrăvița.基于空间分析、沉积物地球化学、原材料、石器分析和 Românești-Dumbrăvița 的使用痕迹的东南欧奥瑞纳文化动态。
Sci Rep. 2022 Aug 19;12(1):14152. doi: 10.1038/s41598-022-15544-5.

本文引用的文献

1
Initial Upper Palaeolithic Homo sapiens from Bacho Kiro Cave, Bulgaria.保加利亚巴乔基罗洞穴的早期旧石器时代智人。
Nature. 2020 May;581(7808):299-302. doi: 10.1038/s41586-020-2259-z. Epub 2020 May 11.
2
A C chronology for the Middle to Upper Palaeolithic transition at Bacho Kiro Cave, Bulgaria.保加利亚 Bacho Kiro 洞穴中、上旧石器时代过渡期的 C 年代测定。
Nat Ecol Evol. 2020 Jun;4(6):794-801. doi: 10.1038/s41559-020-1136-3. Epub 2020 May 11.
3
Heavy reliance on plants for Romanian cave bears evidenced by amino acid nitrogen isotope analysis.
对罗马尼亚洞穴熊的氨基酸氮同位素分析表明，其对植物的高度依赖。
Sci Rep. 2020 Apr 20;10(1):6612. doi: 10.1038/s41598-020-62990-0.
4
SEDIMENTARY RADIOACTIVITY IN AN UPPER PALEOLITHIC-MIDDLE PALEOLITHIC (MP-UP) TRANSITION SITE: INCREASING ESR TOOTH DATING ACCURACY AT GOLEMA PEšT, NORTH MACEDONIA.北马其顿戈莱马佩什特一处旧石器时代晚期 - 旧石器时代中期（MP - UP）过渡遗址的沉积放射性：提高北马其顿戈莱马佩什特的电子自旋共振牙齿测年精度
Radiat Prot Dosimetry. 2019 Dec 31;186(1):94-112. doi: 10.1093/rpd/ncz183.
5
Changing environments during the Middle-Upper Palaeolithic transition in the eastern Cantabrian Region (Spain): direct evidence from stable isotope studies on ungulate bones.中更新世向晚更新世过渡时期坎塔布连地区（西班牙）的环境变化：来自有蹄类动物骨骼稳定同位素研究的直接证据
Sci Rep. 2018 Oct 4;8(1):14842. doi: 10.1038/s41598-018-32493-0.
6
Impact of climate change on the transition of Neanderthals to modern humans in Europe.气候变化对欧洲尼安德特人向现代人过渡的影响。
Proc Natl Acad Sci U S A. 2018 Sep 11;115(37):9116-9121. doi: 10.1073/pnas.1808647115. Epub 2018 Aug 27.
7
On the origin of modern humans: Asian perspectives.现代人的起源：亚洲视角。
Science. 2017 Dec 8;358(6368). doi: 10.1126/science.aai9067.
8
Direct dating of Neanderthal remains from the site of Vindija Cave and implications for the Middle to Upper Paleolithic transition.文迪雅洞穴遗址中尼安德特人遗骸的直接年代测定及其对中-上新世过渡的意义。
Proc Natl Acad Sci U S A. 2017 Oct 3;114(40):10606-10611. doi: 10.1073/pnas.1709235114. Epub 2017 Sep 5.
9
High-precision C and Ar/Ar dating of the Campanian Ignimbrite (Y-5) reconciles the time-scales of climatic-cultural processes at 40 ka.高精度的 C 和 Ar/Ar 年代测定表明，Campanian Ignimbrite（Y-5）与 40 ka 时的气候-文化过程的时间尺度相吻合。
Sci Rep. 2017 Apr 6;7:45940. doi: 10.1038/srep45940.
10
Carbon isotope discrimination by plants follows latitudinal and altitudinal trends.植物的碳同位素分馏呈现出纬度和海拔趋势。
Oecologia. 1991 Sep;88(1):30-40. doi: 10.1007/BF00328400.