RELATIVE SEA-LEVEL CHANGES DURING THE EARLY AND MID-HOLOCENE ON THE COAST OF THE GULF OF LIONS

被引：0

作者：

Salell, Tiphaine ^{[1
,2
]}

Flaux, Clement ^{[3
]}

Bruneton, Helene ^{[4
]}

Degeai, Jean-Philippe ^{[1
,2
]}

Devillers, Benoit ^{[1
,2
]}

Lefevre, David ^{[1
,2
]}

机构：

[1] Univ Paul Valery Montpellier 3, CNRS, MCC, UMR 5140 ASM, Campus St Charles, FR-34199 Montpellier 05, France

[2] Univ Paul Valery Montpellier 3, LabexARCHIMEDE, ANR 11 LABX 0032 01, Campus St Charles, FR-34199 Montpellier 05, France

[3] Mosa Archeol, FR-34660 Cournonterral, France

[4] Univ Aix Marseille, CNRS, UMR 6635, CEREGE,Europole Mediterraneen Arbois, BP 80, FR-13545 Aix En Provence 04, France

来源：

QUATERNAIRE | 2020年 / 31卷 / 01期

关键词：

near-shore peats; lagoonal deposits; filled ria; Aude river delta; Narbonne; north-western Mediterranean; FRENCH MEDITERRANEAN COAST; HOLOCENE EVOLUTION; FORUM-JULII; RHONE DELTA; RISE; FRANCE; AGE; SUBSIDENCE; LAGOON; AUDE;

D O I：

暂无

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

A relative sea-level rise curve on the Gulf of Lions coast is proposed within the range 9500-6000 cal a BP, a period that is currently not well documented in the region. The selected palaeoenvironmental indicators come from the Narbonne area. The filled ria context favours early marine ingression into palaeo-talwegs during the Early Holocene, the concomitant development of peat marshes in the upstream alluvial plain, and a later transgression on the margins of the ria during the Mid-Holocene. The compilation of data from the Narbonne coast and those available in Gulf of Lions and Catalonia coasts suggests low or no local vertical mobility for the period under discussion.

引用

页码：33 / 44

页数：12

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