Palaeolandscape reconstruction of a shallow coastal embayment in Kattegat, Denmark—influence of sea-level changes during the latest Pleistocene and Holocene

IF 2.3 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Boreas Pub Date : 2026-04-14 Epub Date: 2025-12-26 DOI:10.1111/bor.70047
Katrine Juul Andresen, Lars Ole Boldreel, Ole Bennike, Christof Pearce, Mikkel Fruergaard, Verner Brandbyge Ernstsen, Aart Kroon, Nicole Rita Posth, Marit-Solveig Seidenkrantz
{"title":"Palaeolandscape reconstruction of a shallow coastal embayment in Kattegat, Denmark—influence of sea-level changes during the latest Pleistocene and Holocene","authors":"Katrine Juul Andresen,&nbsp;Lars Ole Boldreel,&nbsp;Ole Bennike,&nbsp;Christof Pearce,&nbsp;Mikkel Fruergaard,&nbsp;Verner Brandbyge Ernstsen,&nbsp;Aart Kroon,&nbsp;Nicole Rita Posth,&nbsp;Marit-Solveig Seidenkrantz","doi":"10.1111/bor.70047","DOIUrl":null,"url":null,"abstract":"<p>Shallow coastal embayments are typical features of former glacial landscapes in parts of Scandinavia and North America. An increasing concern over the impact of accelerating sea-level rise, calls for a better understanding of how coasts respond to sea-level changes. Studying the response of coastal environments, such as submerged embayments, to sea-level changes in the past, can provide important insights into the response of present-day coastlines to future sea-level rise. Kalø Bay is an embayment situated in south-western Kattegat, north of the Aarhus Bay, Denmark. This shallow embayment was influenced by sea-level changes governed by global sea-level rise and glacio-isostatic rebound from the Scandinavian Ice Sheet during the latest Pleistocene and Holocene. In this study, we analyse the palaeolandscape in the bay to identify the depositional succession preserved in the bay and understand the dominant geological processes occurring after the last glaciation in response to sea-level changes. Four major depositional units reflect the variable environment in the bay as it changed from a glacial to proglacial setting through coastal and lagoonal infill stages, and gradually developed into a shallow marine environment as the area was inundated approximately 9–6 cal. ka BP. During a relative sea-level fall in the Mid- and Late Holocene, the deposits in the bay reversed to more coastal facies. Our study highlights the sensitivity of coastal embayments and their dynamic response to sea-level changes. Our results show how the bay changed from a wave-dominated setting in the Early Holocene to a current-dominated setting in the Late Holocene, and how the former glacial landscape and coastal deposits were affected differently by the sea-level rise and associated erosion and redeposition. These results are important for understanding the impacts of future accelerating sea-level rise.</p>","PeriodicalId":9184,"journal":{"name":"Boreas","volume":"55 2","pages":"560-584"},"PeriodicalIF":2.3000,"publicationDate":"2026-04-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/bor.70047","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Boreas","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/bor.70047","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2025/12/26 0:00:00","PubModel":"Epub","JCR":"Q2","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
引用次数: 0

Abstract

Shallow coastal embayments are typical features of former glacial landscapes in parts of Scandinavia and North America. An increasing concern over the impact of accelerating sea-level rise, calls for a better understanding of how coasts respond to sea-level changes. Studying the response of coastal environments, such as submerged embayments, to sea-level changes in the past, can provide important insights into the response of present-day coastlines to future sea-level rise. Kalø Bay is an embayment situated in south-western Kattegat, north of the Aarhus Bay, Denmark. This shallow embayment was influenced by sea-level changes governed by global sea-level rise and glacio-isostatic rebound from the Scandinavian Ice Sheet during the latest Pleistocene and Holocene. In this study, we analyse the palaeolandscape in the bay to identify the depositional succession preserved in the bay and understand the dominant geological processes occurring after the last glaciation in response to sea-level changes. Four major depositional units reflect the variable environment in the bay as it changed from a glacial to proglacial setting through coastal and lagoonal infill stages, and gradually developed into a shallow marine environment as the area was inundated approximately 9–6 cal. ka BP. During a relative sea-level fall in the Mid- and Late Holocene, the deposits in the bay reversed to more coastal facies. Our study highlights the sensitivity of coastal embayments and their dynamic response to sea-level changes. Our results show how the bay changed from a wave-dominated setting in the Early Holocene to a current-dominated setting in the Late Holocene, and how the former glacial landscape and coastal deposits were affected differently by the sea-level rise and associated erosion and redeposition. These results are important for understanding the impacts of future accelerating sea-level rise.

Abstract Image

丹麦卡特加特浅海滩古景观重建——最新更新世和全新世海平面变化的影响
在斯堪的纳维亚半岛和北美的部分地区,浅滩海岸是前冰川景观的典型特征。人们越来越关注海平面加速上升的影响,要求更好地了解海岸如何对海平面变化作出反应。研究沿海环境(如水下海湾)对过去海平面变化的反应,可以为了解当今海岸线对未来海平面上升的反应提供重要的见解。Kalø Bay是位于丹麦奥胡斯湾北部卡特加特西南部的一个海湾。这一浅层隆起受全球海平面上升和斯堪的纳维亚冰盖在最新更新世和全新世的冰川均衡反弹所控制的海平面变化的影响。本研究通过对海湾古景观的分析,确定了海湾保存的沉积演替,并了解末次冰期后发生的主要地质过程对海平面变化的响应。四个主要的沉积单元反映了海湾从冰川到前冰川的变化环境,经历了海岸和泻湖的填充阶段,并在淹没约9-6 cal时逐渐发展为浅海环境。ka BP。在全新世中期和晚期海平面相对下降期间,海湾内的沉积物转向更多的海岸相。我们的研究强调了沿海河口的敏感性及其对海平面变化的动态响应。研究结果揭示了渤海湾从全新世早期以波浪为主导的环境到全新世晚期以水流为主导的环境的变化,以及海平面上升及其相关的侵蚀和再沉积对原冰川景观和海岸沉积物的不同影响。这些结果对于理解未来海平面加速上升的影响非常重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Boreas
Boreas 地学-地球科学综合
CiteScore
5.90
自引率
4.50%
发文量
36
审稿时长
>12 weeks
期刊介绍: Boreas has been published since 1972. Articles of wide international interest from all branches of Quaternary research are published. Biological as well as non-biological aspects of the Quaternary environment, in both glaciated and non-glaciated areas, are dealt with: Climate, shore displacement, glacial features, landforms, sediments, organisms and their habitat, and stratigraphical and chronological relationships. Anticipated international interest, at least within a continent or a considerable part of it, is a main criterion for the acceptance of papers. Besides articles, short items like discussion contributions and book reviews are published.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信
小红书