The Holocene paleo-environmental history of the Gangkou River estuary, Hengchun Peninsula, Taiwan

The Taiwan coastal areas are facing predicted sea-level rise effects in the global climate change context. Better understanding of the mechanisms and forcing factors driving the geomorphological evolution of Taiwan’s coastline is essential. We highlight the potential of small river estuaries as arch...

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Main Authors: Christopher Lüthgens, Lih-Der Ho, Nikolaus Clemenz, Jia-Hong Chen, Chia-Hong Jen, Jiun-Yee Yen, Shyh-Jeng Chyi
Format: Article
Language:English
Published: Chinese Geoscience Union 2018-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Online Access: http://tao.cgu.org.tw/media/k2/attachments/v295p547.pdf
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spelling doaj-153b76fb6485477fafd5a58737c5c1a92020-11-24T21:21:06ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802018-01-0129554757610.3319/TAO.2018.05.07.01The Holocene paleo-environmental history of the Gangkou River estuary, Hengchun Peninsula, TaiwanChristopher LüthgensLih-Der HoNikolaus ClemenzJia-Hong ChenChia-Hong JenJiun-Yee YenShyh-Jeng ChyiThe Taiwan coastal areas are facing predicted sea-level rise effects in the global climate change context. Better understanding of the mechanisms and forcing factors driving the geomorphological evolution of Taiwan’s coastline is essential. We highlight the potential of small river estuaries as archives of coastal evolution and provide a paleo-environmental reconstruction of the Gangkou River estuary based on results from a combined methodological approach using geomorphological, sedimentological, and geochronological analyses. A consistent chronology was established by combining Optically Stimulated Luminescence (OSL) dating, as well as radiocarbon dating techniques. A distinct beach-rock layer allowed firm correlation of six investigated coastal profiles. Eustatic sea level change was identified as the primary coastal and estuarine landscape development forcing factor in the study area. Tectonic forcing could also be detected from the investigated sites, but has to be regarded as a subordinate secondary forcing factor. The Gangkou River estuary developed in the early Holocene at about 8 ka and was fully developed by the time the Holocene sea-level maximum was reached. With the sea-level dropping until modern times, estuarine zone relocation and a transition to terrestrial processes was initiated, leading to development of the current coastal dune system since about 2.5 ka. Major dune building phases correlate with the climate change associated with the Little Ice Age (LIA) event and stabilised towards recent times, which is in accordance with regional and over-regional coastal Aeolian records in Taiwan. http://tao.cgu.org.tw/media/k2/attachments/v295p547.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Christopher Lüthgens
Lih-Der Ho
Nikolaus Clemenz
Jia-Hong Chen
Chia-Hong Jen
Jiun-Yee Yen
Shyh-Jeng Chyi
spellingShingle Christopher Lüthgens
Lih-Der Ho
Nikolaus Clemenz
Jia-Hong Chen
Chia-Hong Jen
Jiun-Yee Yen
Shyh-Jeng Chyi
The Holocene paleo-environmental history of the Gangkou River estuary, Hengchun Peninsula, Taiwan
Terrestrial, Atmospheric and Oceanic Sciences
author_facet Christopher Lüthgens
Lih-Der Ho
Nikolaus Clemenz
Jia-Hong Chen
Chia-Hong Jen
Jiun-Yee Yen
Shyh-Jeng Chyi
author_sort Christopher Lüthgens
title The Holocene paleo-environmental history of the Gangkou River estuary, Hengchun Peninsula, Taiwan
title_short The Holocene paleo-environmental history of the Gangkou River estuary, Hengchun Peninsula, Taiwan
title_full The Holocene paleo-environmental history of the Gangkou River estuary, Hengchun Peninsula, Taiwan
title_fullStr The Holocene paleo-environmental history of the Gangkou River estuary, Hengchun Peninsula, Taiwan
title_full_unstemmed The Holocene paleo-environmental history of the Gangkou River estuary, Hengchun Peninsula, Taiwan
title_sort holocene paleo-environmental history of the gangkou river estuary, hengchun peninsula, taiwan
publisher Chinese Geoscience Union
series Terrestrial, Atmospheric and Oceanic Sciences
issn 1017-0839
2311-7680
publishDate 2018-01-01
description The Taiwan coastal areas are facing predicted sea-level rise effects in the global climate change context. Better understanding of the mechanisms and forcing factors driving the geomorphological evolution of Taiwan’s coastline is essential. We highlight the potential of small river estuaries as archives of coastal evolution and provide a paleo-environmental reconstruction of the Gangkou River estuary based on results from a combined methodological approach using geomorphological, sedimentological, and geochronological analyses. A consistent chronology was established by combining Optically Stimulated Luminescence (OSL) dating, as well as radiocarbon dating techniques. A distinct beach-rock layer allowed firm correlation of six investigated coastal profiles. Eustatic sea level change was identified as the primary coastal and estuarine landscape development forcing factor in the study area. Tectonic forcing could also be detected from the investigated sites, but has to be regarded as a subordinate secondary forcing factor. The Gangkou River estuary developed in the early Holocene at about 8 ka and was fully developed by the time the Holocene sea-level maximum was reached. With the sea-level dropping until modern times, estuarine zone relocation and a transition to terrestrial processes was initiated, leading to development of the current coastal dune system since about 2.5 ka. Major dune building phases correlate with the climate change associated with the Little Ice Age (LIA) event and stabilised towards recent times, which is in accordance with regional and over-regional coastal Aeolian records in Taiwan.
url http://tao.cgu.org.tw/media/k2/attachments/v295p547.pdf
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