Skip to main content

ETHNOS_APP

Home • Search • Journals • List 0

Carles Pelejero

Biographic Data

ID6227284
NAMECarles Pelejero
GIVEN NAMESCarles
FAMILY NAMEPelejero
SIGNATUREPELEJERO C
AFFILIATIONSUniversidad de Salamanca
ORCID0000-0002-7763-7769
VERIFIEDYes
TOTAL WORKS3
TOTAL CITATIONS4
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1999
LATEST PUBLICATION YEAR2021
H-INDEX1
  • Uncoupled seasonal variability of transparent exopolymer and Coomassie stainable particles in coastal Mediterranean waters

    Open Access•Marina Zamanillo, Eva Ortega-Retuerta et al.•ARTICLE•Elementa Science of the…•2021

    Transparent exopolymer particles (TEP) and Coomassie stainable particles (CSP) are gel-like particles, ubiquitous in the ocean, that affect important biogeochemical processes including organic carbon cycling by planktonic food webs. Despite much research on both groups of particles (especially TEP) over many years, whether they exist as distinctly stainable fractions of the same particles or as independent particles, each with different driving f…

  • The last 3000 years in the Ría de Vigo (NW Iberian Margin)

    Open Access•Paula Diz, Guillermo Francés et al.•ARTICLE•The Holocene•2002•Cited by: 4•References: 3

    The hydrographic evolution of the Ria de Vigo (NW Spain) during the last 3000 years has been reconstructed using benthic foraminiferal assemblages, stable oxygen isotopes, molecular biomarkers and seasurface temperatures (SST) reconstructed from the U K 37 index. Benthic oxygen isotopes and SST records provide evidence of episodic salinity contrasts between surface and bottom waters. The comparison of SSTs with other climate records for the North…

  • Dansgaard‐Oeschger and Heinrich event imprints in Alboran Sea paleotemperatures

    Open Access•Isabel Cacho, Joan O Grimalt et al.•ARTICLE•Paleoceanography•1999

    Past sea surface temperature (SST) evolution in the Alboran Sea (western Mediterranean) during the last 50,000 years has been inferred from the study of C 37 alkenones in International Marine Global Change Studies MD952043 core. This record has a time resolution of ∼200 years allowing the study of millennial‐scale and even shorter climatic changes. The observed SST curve displays characteristic sequences of extremely rapid warming and cooling eve…

  • The last 3000 years in the Ría de Vigo (NW Iberian Margin)

    Open Access•Paula Diz, Guillermo Francés et al.•ARTICLE•The Holocene•2002•Cited by: 4•References: 3

    The hydrographic evolution of the Ria de Vigo (NW Spain) during the last 3000 years has been reconstructed using benthic foraminiferal assemblages, stable oxygen isotopes, molecular biomarkers and seasurface temperatures (SST) reconstructed from the U K 37 index. Benthic oxygen isotopes and SST records provide evidence of episodic salinity contrasts between surface and bottom waters. The comparison of SSTs with other climate records for the North…

  • Dansgaard‐Oeschger and Heinrich event imprints in Alboran Sea paleotemperatures

    Open Access•Isabel Cacho, Joan O Grimalt et al.•ARTICLE•Paleoceanography•1999

    Past sea surface temperature (SST) evolution in the Alboran Sea (western Mediterranean) during the last 50,000 years has been inferred from the study of C 37 alkenones in International Marine Global Change Studies MD952043 core. This record has a time resolution of ∼200 years allowing the study of millennial‐scale and even shorter climatic changes. The observed SST curve displays characteristic sequences of extremely rapid warming and cooling eve…

  • The last 3000 years in the Ría de Vigo (NW Iberian Margin)

    Open Access•Paula Diz, Guillermo Francés et al.•ARTICLE•The Holocene•2002•Cited by: 4•References: 3

    The hydrographic evolution of the Ria de Vigo (NW Spain) during the last 3000 years has been reconstructed using benthic foraminiferal assemblages, stable oxygen isotopes, molecular biomarkers and seasurface temperatures (SST) reconstructed from the U K 37 index. Benthic oxygen isotopes and SST records provide evidence of episodic salinity contrasts between surface and bottom waters. The comparison of SSTs with other climate records for the North…

  • Uncoupled seasonal variability of transparent exopolymer and Coomassie stainable particles in coastal Mediterranean waters

    Open Access•Marina Zamanillo, Eva Ortega-Retuerta et al.•ARTICLE•Elementa Science of the…•2021

    Transparent exopolymer particles (TEP) and Coomassie stainable particles (CSP) are gel-like particles, ubiquitous in the ocean, that affect important biogeochemical processes including organic carbon cycling by planktonic food webs. Despite much research on both groups of particles (especially TEP) over many years, whether they exist as distinctly stainable fractions of the same particles or as independent particles, each with different driving f…

Environmental Science (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Hydrography (2 works) · Oceanography (2 works) · Plankton (2 works) · Bay (1 work) · Benthic zone (1 work) · Biogeochemical cycle (1 work) · Biology (1 work)

Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae