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David Domínguez-Villar

Biographic Data

ID1542402
NAMEDavid Domínguez-Villar
GIVEN NAMESDavid
FAMILY NAMEDomínguez-Villar
SIGNATUREDOMÍNGUEZ-VILLAR D
AFFILIATIONSUniversidad de Salamanca
VERIFIEDNo
TOTAL WORKS10
TOTAL CITATIONS1
AUTHOR COUNT10
EDITOR COUNT0
FIRST PUBLICATION YEAR2008
LATEST PUBLICATION YEAR2026
H-INDEX1
  • Investigations of short-term denudation rates on the North Dalmatian Plain (Croatia)

    Open Access•Kristina Krklec, Dražen Perica et al.•ARTICLE•Quaternary International•2026•References: 63

    Studies of denudation rates in carbonate areas are an important step to understand rates of karst landscape development. Weathering of carbonate rocks is an essential process in soil formation and has a significant role in the global CO 2 budget. We studied short-term weathering and denudation rates at a location in the Dinaric karst using the rock tablet method while monitoring surficial and soil environmental parameters. We exposed “standard” r…

  • Thermal impact of Heinrich stadials in cave temperature and speleothem oxygen isotope records

    Open Access•David Domínguez-Villar, David Domínguez‐villar et al.•ARTICLE•Quaternary Research•2021

    During each Heinrich stadial (HS), temperatures in southern Europe typically dropped several degrees during several hundred to few thousand years. We have developed a one-dimensional thermal conduction model that transfers the typical surface temperature anomaly of a HS to a series of hypothetical underlying caves. The results show that with increasing depth, the thermal anomaly is attenuated, the lag time increases, and the signal structure expe…

  • Climate change going deep

    Open Access•Stefano Mammola, Elena Piano et al.•ARTICLE•The Anthropocene Review•2019•Cited by: 1•References: 126

    Scientists of different disciplines have recognized the valuable role of terrestrial caves as ideal natural laboratories in which to study multiple eco-evolutionary processes, from genes to ecosystems. Because caves and other subterranean habitats are semi-closed systems characterized by a remarkable thermal stability, they should also represent insightful systems for understanding the effects of climate change on biodiversity in situ. Whilst a n…

  • Morphometric comparison of weathering features on side by side carbonate rock surfaces with different exposure ages ― A case from the Croatian coast

    Open Access•Kristina Krklec, David Domínguez-Villar et al.•ARTICLE•Quaternary International•2018

  • Late Pleistocene glacial evolutionary stages in the Gredos Mountains (Iberian Central System)

    Javier Pedraza, Rosa M Carrasco et al.•ARTICLE•Quaternary International•2013

  • Weathering phases recorded by gnammas

    Open Access•David Domínguez-Villar, David Domínguez‐villar et al.•ARTICLE•Quaternary Research•2012

  • Comparison of the amount of rainfall between the Eemian and the Holocene and the turbulent transition to the last interglacial period recorded in freshwater tufas from Central Spain

    Open Access•David Domínguez-Villar•ARTICLE•Quaternary International•2012

  • Oxygen isotope record from 33 to 9 ka BP based on stalagmites from Eagle Cave, Spain

    Open Access•David Domínguez-Villar•ARTICLE•Quaternary International•2012

  • Weathering phases recorded by gnammas developed since last glaciation at Serra da Estrela, Portugal

    Open Access•David Domínguez-Villar, David Domínguez‐villar et al.•ARTICLE•Quaternary Research•2009

    The morphometrical analysis of gnammas (weathering pits) in granite landscapes has been used to establish the relative chronology of recent erosive surfaces and to provide the weathering history in a region. To test the validity of gnammas as relative chronometer indicators, and the reliability of the obtained weathering record, two sites have been studied in Serra da Estrela, Portugal. The first site is within the limits of the glacier that exis…

  • Α high-resolution late Holocene speleothem record from Kaite Cave, northern Spain

    Open Access•David Domínguez-Villar, Xianfeng Wang et al.•ARTICLE•Quaternary International•2008

  • Climate change going deep

    Open Access•Stefano Mammola, Elena Piano et al.•ARTICLE•The Anthropocene Review•2019•Cited by: 1•References: 126

    Scientists of different disciplines have recognized the valuable role of terrestrial caves as ideal natural laboratories in which to study multiple eco-evolutionary processes, from genes to ecosystems. Because caves and other subterranean habitats are semi-closed systems characterized by a remarkable thermal stability, they should also represent insightful systems for understanding the effects of climate change on biodiversity in situ. Whilst a n…

  • Α high-resolution late Holocene speleothem record from Kaite Cave, northern Spain

    Open Access•David Domínguez-Villar, Xianfeng Wang et al.•ARTICLE•Quaternary International•2008

  • Weathering phases recorded by gnammas developed since last glaciation at Serra da Estrela, Portugal

    Open Access•David Domínguez-Villar, David Domínguez‐villar et al.•ARTICLE•Quaternary Research•2009

    The morphometrical analysis of gnammas (weathering pits) in granite landscapes has been used to establish the relative chronology of recent erosive surfaces and to provide the weathering history in a region. To test the validity of gnammas as relative chronometer indicators, and the reliability of the obtained weathering record, two sites have been studied in Serra da Estrela, Portugal. The first site is within the limits of the glacier that exis…

  • Weathering phases recorded by gnammas

    Open Access•David Domínguez-Villar, David Domínguez‐villar et al.•ARTICLE•Quaternary Research•2012

  • Comparison of the amount of rainfall between the Eemian and the Holocene and the turbulent transition to the last interglacial period recorded in freshwater tufas from Central Spain

    Open Access•David Domínguez-Villar•ARTICLE•Quaternary International•2012

  • Oxygen isotope record from 33 to 9 ka BP based on stalagmites from Eagle Cave, Spain

    Open Access•David Domínguez-Villar•ARTICLE•Quaternary International•2012

  • Late Pleistocene glacial evolutionary stages in the Gredos Mountains (Iberian Central System)

    Javier Pedraza, Rosa M Carrasco et al.•ARTICLE•Quaternary International•2013

  • Morphometric comparison of weathering features on side by side carbonate rock surfaces with different exposure ages ― A case from the Croatian coast

    Open Access•Kristina Krklec, David Domínguez-Villar et al.•ARTICLE•Quaternary International•2018

  • Climate change going deep

    Open Access•Stefano Mammola, Elena Piano et al.•ARTICLE•The Anthropocene Review•2019•Cited by: 1•References: 126

    Scientists of different disciplines have recognized the valuable role of terrestrial caves as ideal natural laboratories in which to study multiple eco-evolutionary processes, from genes to ecosystems. Because caves and other subterranean habitats are semi-closed systems characterized by a remarkable thermal stability, they should also represent insightful systems for understanding the effects of climate change on biodiversity in situ. Whilst a n…

  • Thermal impact of Heinrich stadials in cave temperature and speleothem oxygen isotope records

    Open Access•David Domínguez-Villar, David Domínguez‐villar et al.•ARTICLE•Quaternary Research•2021

    During each Heinrich stadial (HS), temperatures in southern Europe typically dropped several degrees during several hundred to few thousand years. We have developed a one-dimensional thermal conduction model that transfers the typical surface temperature anomaly of a HS to a series of hypothetical underlying caves. The results show that with increasing depth, the thermal anomaly is attenuated, the lag time increases, and the signal structure expe…

  • Investigations of short-term denudation rates on the North Dalmatian Plain (Croatia)

    Open Access•Kristina Krklec, Dražen Perica et al.•ARTICLE•Quaternary International•2026•References: 63

    Studies of denudation rates in carbonate areas are an important step to understand rates of karst landscape development. Weathering of carbonate rocks is an essential process in soil formation and has a significant role in the global CO 2 budget. We studied short-term weathering and denudation rates at a location in the Dinaric karst using the rock tablet method while monitoring surficial and soil environmental parameters. We exposed “standard” r…

Geology and Paleoclimatology Research (7 works) · Geology (6 works) · Geography (5 works) · Paleontology (5 works) · Cave (4 works) · Geochemistry (4 works) · Karst Systems and Hydrogeology (4 works) · Archaeology (3 works) · Climate change (3 works) · Climatology (3 works)

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