The Taravilla lake and tufa deposits (Central Iberian Range, Spain) as palaeohydrological and palaeoclimatic indicators

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 259, Issue 2-3, 2008, Pages 136-156

  Valero Garces B L ^a   Moreno, A ^a   Navas, A ^b   Mata, P ^c   Machin J ^b   Delgado Huertas, A ^d   Gonzalez Samperiz P ^a   Schwalb, A ^e   Morellon M ^a   Cheng, Hai ^f   Edwards, R L ^f  

^a INSTITUTO PIRENAICO DE ECOLOGÍA   (Spain)

^b CSIC   (Spain)

^c UNIVERSITY OF CÁDIZ   (Spain)

^d CSIC   (Spain)

^e TECHNICAL UNIVERSITY OF BRAUNSCHWEIG   (Germany)

^f UNIVERSITY OF MINNESOTA   (United States)

Author keywords

Holocene; karstic; lake; Mediterranean; palaeoclimate; Spain; stable isotope; tufa

Indexed keywords

CHRONOLOGY; ENVIRONMENTAL CHANGE; FLOOD; HOLOCENE; ISOTOPIC COMPOSITION; LACUSTRINE ENVIRONMENT; LAKE WATER; LATE GLACIAL; LITTLE ICE AGE; PALEOCLIMATE; PALEOHYDROLOGY; SEDIMENT CORE; SPRING WATER; STABLE ISOTOPE; TUFA; VALLEY;

CASTILLA-LA MANCHA; EURASIA; EUROPE; GUADALAJARA [CASTILLA-LA MANCHA]; IBERIAN CORDILLERA; SOUTHERN EUROPE; SPAIN; TARAVILLA LAKE;

OSTRACODA;

EID: 40049099089     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2007.10.004     Document Type: Article

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