Holocene palaeoenvironmental evolution of Salt,s Island (Tinto and Odiel estuary, SW Spain) during the Roman period (1st century BC-5th century AD)

被引：4

作者：

Gonzalez-Regalado, Maria L. ^{[1
]}

Gomez, Paula ^{[1
,8
]}

Ruiz, Francisco ^{[1
,8
]}

Caceres, Luis M. ^{[1
,8
]}

Clemente, Maria J. ^{[1
,8
]}

Rodriguez-Vidal, Joaquin ^{[1
,8
]}

Toscano, Antonio ^{[1
,8
]}

Monge, Guadalupe ^{[2
]}

Abad, Manuel ^{[3
,8
]}

Izquierdo, Tatiana ^{[3
,8
]}

Monge Soares, Antonio M. ^{[4
]}

Campos, Juan M. ^{[5
,8
]}

Bermejo, Javier ^{[5
,8
]}

Martinez-Aguirre, Aranzazu ^{[6
]}

Lopez, Gloria I. ^{[7
]}

机构：

[1] Univ Huelva, Dept Ciencias Tierra, Avda Tres Marzo S-N, Huelva 21071, Spain

[2] Univ Seville, Dept Cristalog Mineral & Quim Agr, Seville 41071, Spain

[3] Univ Atacama, Avda Copayapu 485, Copiapo, Chile

[4] Univ Lisbon, Inst Super Tecn, C2TN, Bobadela LRS, Estr Nacl 10,K 139-7, P-2695066 Lisbon, Portugal

[5] Univ Huelva, Dept Hist 1, Avda Tres Marzo S-N, Huelva 21071, Spain

[6] Univ Seville, EUITA, Dept Fis Aplicada 1, Crta Utrera Km 1, Seville 41013, Spain

[7] Ctr Nacl Invest Evoluc Humana, Paseo Sierra Atapuerca 3, Burgos 09002, Spain

[8] Univ Huelva, CIPHCN, Fac Humanidades, Avda Tres Marzo S-N, Huelva 21071, Spain

来源：

JOURNAL OF IBERIAN GEOLOGY | 2019年 / 45卷 / 01期

关键词：

Sedimentary facies; Palaeontology; Archaeology; Roman evolution; Holocene palaeoenviromental reconstruction; Tinto-Odiel estuary; HIGH-ENERGY EVENTS; CHENIER-PLAIN; SEA-LEVEL; GEOLOGICAL RECORD; RIVER MOUTH; FORAMINIFERA; CADIZ; COAST; BAY; ASSEMBLAGES;

D O I：

10.1007/s41513-018-0089-8

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

A multidisciplinary analysis of Holocene sediments from Salt,s Island (Tinto-Odiel estuary, SW Spain) has allowed to differentiate eigth sedimentary facies, according to their textural characteristics, internal structure, paleontology and archaeological content. Its interpretation and the chronological datings carried out reconstruct a transition from a sandy tidal plain to a final occupation by a Roman salting (cetaria) between the 1st century BC to 5th century A. This evolution includes the deposit of washover fans derived from high-energy events between the 1st century BC to 3th century AD. The integration of these new data with others from previous research has allowed partially complete the palaeoenviromental reconstruction of the marine domain of the Tinto-Odiel estuary.

引用

页码：129 / 145

页数：17

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