Mid and Late Holocene evolution of Brateș Lake region (Danube floodplain) based on the multiproxy analysis

This study proposes a local paleo–landscape reconstruction of the Danube floodplain based on a stratigraphic sequence retrieved from Brateș Lake which, by its emplacement near the confluence of Danube – Prut rivers, was fully receptive to changes associated to hydrological, geomorphological or anthr...
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Gespeichert in:

Autor*in:	Laurențiu ȚUȚUIANU [verfasserIn] Alfred VESPREMEANU–STROE [verfasserIn] Florin PENDEA [verfasserIn] Tiberiu SAVA [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch ; Französisch

Erschienen:	2018

Schlagwörter:	landscape changes aggradation chronology stratigraphy units

Übergeordnetes Werk:	In: Revista de Geomorfologie - Romanian Association of Geomorphologists, 2021, 20(2018), 1
Übergeordnetes Werk:	volume:20 ; year:2018 ; number:1

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.21094/rg.2018.017

Katalog-ID:	DOAJ070123349

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callnumber-first	G - Geography, Anthropology, Recreation
author	Laurențiu ȚUȚUIANU
spellingShingle	Laurențiu ȚUȚUIANU misc G1-922 misc landscape changes misc aggradation misc chronology misc stratigraphy units misc Geography (General) Mid and Late Holocene evolution of Brateș Lake region (Danube floodplain) based on the multiproxy analysis
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topic_title	G1-922 Mid and Late Holocene evolution of Brateș Lake region (Danube floodplain) based on the multiproxy analysis landscape changes aggradation chronology stratigraphy units
topic	misc G1-922 misc landscape changes misc aggradation misc chronology misc stratigraphy units misc Geography (General)
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title	Mid and Late Holocene evolution of Brateș Lake region (Danube floodplain) based on the multiproxy analysis
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title_full	Mid and Late Holocene evolution of Brateș Lake region (Danube floodplain) based on the multiproxy analysis
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title_sort	mid and late holocene evolution of brateș lake region (danube floodplain) based on the multiproxy analysis
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title_auth	Mid and Late Holocene evolution of Brateș Lake region (Danube floodplain) based on the multiproxy analysis
abstract	This study proposes a local paleo–landscape reconstruction of the Danube floodplain based on a stratigraphic sequence retrieved from Brateș Lake which, by its emplacement near the confluence of Danube – Prut rivers, was fully receptive to changes associated to hydrological, geomorphological or anthropogenic driven events. Due to its intermediate position within the Lower Danube valley Brateș Lake is a proxy for the evolution of Cotul Dunării area (the region of Danube valley turning from S–N to W–E direction) and provide valuable information about the timing of Danube river advancement to the Black Sea after its reconnection to World Ocean. The sediments were analysed to get the history of their deposition by means of accelerator mass spectrometry (AMS) 14C dating, grain–size parameters, organic matter and carbonate content, magnetic susceptibility together with paleo–fauna and pollen content which altogether led to the identification of main stages: i) delta front advance into Danube estuary (before 8000 BP), ii) shoreline foreshore deposits which describe shoreline position (8000–7900 yrs BP), iii) river floodplain development (7900–5300/5000 yrs BP), iv) lake formation (5300/5000 yrs BP – present).
abstractGer	This study proposes a local paleo–landscape reconstruction of the Danube floodplain based on a stratigraphic sequence retrieved from Brateș Lake which, by its emplacement near the confluence of Danube – Prut rivers, was fully receptive to changes associated to hydrological, geomorphological or anthropogenic driven events. Due to its intermediate position within the Lower Danube valley Brateș Lake is a proxy for the evolution of Cotul Dunării area (the region of Danube valley turning from S–N to W–E direction) and provide valuable information about the timing of Danube river advancement to the Black Sea after its reconnection to World Ocean. The sediments were analysed to get the history of their deposition by means of accelerator mass spectrometry (AMS) 14C dating, grain–size parameters, organic matter and carbonate content, magnetic susceptibility together with paleo–fauna and pollen content which altogether led to the identification of main stages: i) delta front advance into Danube estuary (before 8000 BP), ii) shoreline foreshore deposits which describe shoreline position (8000–7900 yrs BP), iii) river floodplain development (7900–5300/5000 yrs BP), iv) lake formation (5300/5000 yrs BP – present).
abstract_unstemmed	This study proposes a local paleo–landscape reconstruction of the Danube floodplain based on a stratigraphic sequence retrieved from Brateș Lake which, by its emplacement near the confluence of Danube – Prut rivers, was fully receptive to changes associated to hydrological, geomorphological or anthropogenic driven events. Due to its intermediate position within the Lower Danube valley Brateș Lake is a proxy for the evolution of Cotul Dunării area (the region of Danube valley turning from S–N to W–E direction) and provide valuable information about the timing of Danube river advancement to the Black Sea after its reconnection to World Ocean. The sediments were analysed to get the history of their deposition by means of accelerator mass spectrometry (AMS) 14C dating, grain–size parameters, organic matter and carbonate content, magnetic susceptibility together with paleo–fauna and pollen content which altogether led to the identification of main stages: i) delta front advance into Danube estuary (before 8000 BP), ii) shoreline foreshore deposits which describe shoreline position (8000–7900 yrs BP), iii) river floodplain development (7900–5300/5000 yrs BP), iv) lake formation (5300/5000 yrs BP – present).
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title_short	Mid and Late Holocene evolution of Brateș Lake region (Danube floodplain) based on the multiproxy analysis
url	https://doi.org/10.21094/rg.2018.017 https://doaj.org/article/08a1fbec882c4eaeaf40d1cc8720ea4e http://revistadegeomorfologie.ro/geo/index.php/revista/article/view/35 https://doaj.org/toc/1453-5068 https://doaj.org/toc/2285-6773
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up_date	2024-07-04T01:55:06.026Z
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Mid and Late Holocene evolution of Brateș Lake region (Danube floodplain) based on the multiproxy analysis

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