Late Quaternary Palaeoclimate Reconstruction Based on Clay Minerals Assemblage from Preluca Tiganului (Gutai Mountains, Romania)

Lucreția Ghergari; Bogdan P. Onac

doi:10.5038/1937-8602.46.1.2

Late Quaternary Palaeoclimate Reconstruction Based on Clay Minerals Assemblage from Preluca Tiganului (Gutai Mountains, Romania)

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Abstract

Several core samples were extracted from the overgrown crater lake of Preluca Tiganului, NW Romania. The overall lithology and the mineral assemblages (mostly clay) described from different levels within these cores, suggest three main periods having humid or dry conditions. Based on these findings, palaeoclimate conditions can be reconstructed the over the time period spanning 15,000 to 13,500 cal. years BP.

Original language	American English
Journal	Default journal
DOIs	https://doi.org/10.5038/1937-8602.46.1.2
State	Published - 1800
Externally published	Yes

Keywords

Late Quaternary
palaeoclimate
clay minerals
Preluca Tiganului crater
Gutâi Mountains
Romania

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10.5038/1937-8602.46.1.2License: CC BY

Late Quaternary Palaeoclimate Reconstruction Based on Clay MineraFinal published version, 1.9 MBLicense: CC BY

Cite this

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title = "Late Quaternary Palaeoclimate Reconstruction Based on Clay Minerals Assemblage from Preluca Tiganului (Gutai Mountains, Romania)",

abstract = " Several core samples were extracted from the overgrown crater lake of Preluca Tiganului, NW Romania. The overall lithology and the mineral assemblages (mostly clay) described from different levels within these cores, suggest three main periods having humid or dry conditions. Based on these findings, palaeoclimate conditions can be reconstructed the over the time period spanning 15,000 to 13,500 cal. years BP.",

keywords = "Late Quaternary, palaeoclimate, clay minerals, Preluca Tiganului crater, Gut{\^a}i Mountains, Romania",

author = "Lucreția Ghergari and Onac, {Bogdan P.}",

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doi = "10.5038/1937-8602.46.1.2",

language = "American English",

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AU - Ghergari, Lucreția

AU - Onac, Bogdan P.

PY - 1800

Y1 - 1800

N2 - Several core samples were extracted from the overgrown crater lake of Preluca Tiganului, NW Romania. The overall lithology and the mineral assemblages (mostly clay) described from different levels within these cores, suggest three main periods having humid or dry conditions. Based on these findings, palaeoclimate conditions can be reconstructed the over the time period spanning 15,000 to 13,500 cal. years BP.

AB - Several core samples were extracted from the overgrown crater lake of Preluca Tiganului, NW Romania. The overall lithology and the mineral assemblages (mostly clay) described from different levels within these cores, suggest three main periods having humid or dry conditions. Based on these findings, palaeoclimate conditions can be reconstructed the over the time period spanning 15,000 to 13,500 cal. years BP.

KW - Late Quaternary

KW - palaeoclimate

KW - clay minerals

KW - Preluca Tiganului crater

KW - Gutâi Mountains

KW - Romania

UR - https://digitalcommons.usf.edu/geologia/vol46/iss1/art2

U2 - 10.5038/1937-8602.46.1.2

DO - 10.5038/1937-8602.46.1.2

M3 - Article

JO - Default journal

JF - Default journal

ER -

Late Quaternary Palaeoclimate Reconstruction Based on Clay Minerals Assemblage from Preluca Tiganului (Gutai Mountains, Romania)

Abstract

Keywords

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