Organic carbon (OC) and carbon isotope ratio (δ13C) in sediment cores from the Gulf of Cádiz (North East Atlantic)
Organic carbon (OC), total nitrogen (TN), and carbon isotope ratio (δ13C) were measured in sediment cores to constrain the relative contribution of marine and terrestrial sources of organic matter (OM) in the continental shelf of the Gulf of Cádiz. Five sampling stations were selected in two differe...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.918394 2023-05-15T17:38:17+02:00 Organic carbon (OC) and carbon isotope ratio (δ13C) in sediment cores from the Gulf of Cádiz (North East Atlantic) Guerra, Roberta Garcia-Luque, Enrique MEDIAN LATITUDE: 36.640380 * MEDIAN LONGITUDE: -6.488450 * SOUTH-BOUND LATITUDE: 36.551500 * WEST-BOUND LONGITUDE: -6.667600 * NORTH-BOUND LATITUDE: 36.789700 * EAST-BOUND LONGITUDE: -6.325640 * DATE/TIME START: 2006-06-20T00:00:00 * DATE/TIME END: 2006-11-26T00:00:00 2020-06-05 application/zip, 5 datasets https://doi.pangaea.de/10.1594/PANGAEA.918394 https://doi.org/10.1594/PANGAEA.918394 en eng PANGAEA Guerra, Roberta; Righi, Serena; Garcia-Luque, Enrique (2015): Modern accumulation rates and sources of organic carbon in the NE Gulf of Cádiz (SW Iberian Peninsula). Journal of Radioanalytical and Nuclear Chemistry, 305(2), 429-437, https://doi.org/10.1007/s10967-015-3991-y https://doi.pangaea.de/10.1594/PANGAEA.918394 https://doi.org/10.1594/PANGAEA.918394 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY carbon isotope ratio (δ13C) EMIGAS Greenhouse gas emission zones in coastal systems: influence of coastal runoff and benthic metabolism Gulf of Cadiz North East Atlantic organic carbon (OC) sediment Dataset 2020 ftpangaea https://doi.org/10.1594/PANGAEA.918394 https://doi.org/10.1007/s10967-015-3991-y 2023-01-20T07:34:33Z Organic carbon (OC), total nitrogen (TN), and carbon isotope ratio (δ13C) were measured in sediment cores to constrain the relative contribution of marine and terrestrial sources of organic matter (OM) in the continental shelf of the Gulf of Cádiz. Five sampling stations were selected in two different areas: the Bay of Cádiz and its outer region (BOX BC02, BOX BC04, BOX BC05), and the Guadalquivir prodelta (BOX GL03, BOX GL04), which is characterized by a high fluvial supply and a moderate hydrodynamic regime. C/N and δ13C data show that sedimentary OM is a mixture of marine and terrigenous OM with larger contributions from marine sources in the Bay of Cádiz, and terrestrial sources in the Guadalquivir prodelta. Dataset North East Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-6.667600,-6.325640,36.789700,36.551500) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
carbon isotope ratio (δ13C) EMIGAS Greenhouse gas emission zones in coastal systems: influence of coastal runoff and benthic metabolism Gulf of Cadiz North East Atlantic organic carbon (OC) sediment |
spellingShingle |
carbon isotope ratio (δ13C) EMIGAS Greenhouse gas emission zones in coastal systems: influence of coastal runoff and benthic metabolism Gulf of Cadiz North East Atlantic organic carbon (OC) sediment Guerra, Roberta Garcia-Luque, Enrique Organic carbon (OC) and carbon isotope ratio (δ13C) in sediment cores from the Gulf of Cádiz (North East Atlantic) |
topic_facet |
carbon isotope ratio (δ13C) EMIGAS Greenhouse gas emission zones in coastal systems: influence of coastal runoff and benthic metabolism Gulf of Cadiz North East Atlantic organic carbon (OC) sediment |
description |
Organic carbon (OC), total nitrogen (TN), and carbon isotope ratio (δ13C) were measured in sediment cores to constrain the relative contribution of marine and terrestrial sources of organic matter (OM) in the continental shelf of the Gulf of Cádiz. Five sampling stations were selected in two different areas: the Bay of Cádiz and its outer region (BOX BC02, BOX BC04, BOX BC05), and the Guadalquivir prodelta (BOX GL03, BOX GL04), which is characterized by a high fluvial supply and a moderate hydrodynamic regime. C/N and δ13C data show that sedimentary OM is a mixture of marine and terrigenous OM with larger contributions from marine sources in the Bay of Cádiz, and terrestrial sources in the Guadalquivir prodelta. |
format |
Dataset |
author |
Guerra, Roberta Garcia-Luque, Enrique |
author_facet |
Guerra, Roberta Garcia-Luque, Enrique |
author_sort |
Guerra, Roberta |
title |
Organic carbon (OC) and carbon isotope ratio (δ13C) in sediment cores from the Gulf of Cádiz (North East Atlantic) |
title_short |
Organic carbon (OC) and carbon isotope ratio (δ13C) in sediment cores from the Gulf of Cádiz (North East Atlantic) |
title_full |
Organic carbon (OC) and carbon isotope ratio (δ13C) in sediment cores from the Gulf of Cádiz (North East Atlantic) |
title_fullStr |
Organic carbon (OC) and carbon isotope ratio (δ13C) in sediment cores from the Gulf of Cádiz (North East Atlantic) |
title_full_unstemmed |
Organic carbon (OC) and carbon isotope ratio (δ13C) in sediment cores from the Gulf of Cádiz (North East Atlantic) |
title_sort |
organic carbon (oc) and carbon isotope ratio (δ13c) in sediment cores from the gulf of cádiz (north east atlantic) |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.918394 https://doi.org/10.1594/PANGAEA.918394 |
op_coverage |
MEDIAN LATITUDE: 36.640380 * MEDIAN LONGITUDE: -6.488450 * SOUTH-BOUND LATITUDE: 36.551500 * WEST-BOUND LONGITUDE: -6.667600 * NORTH-BOUND LATITUDE: 36.789700 * EAST-BOUND LONGITUDE: -6.325640 * DATE/TIME START: 2006-06-20T00:00:00 * DATE/TIME END: 2006-11-26T00:00:00 |
long_lat |
ENVELOPE(-6.667600,-6.325640,36.789700,36.551500) |
genre |
North East Atlantic |
genre_facet |
North East Atlantic |
op_relation |
Guerra, Roberta; Righi, Serena; Garcia-Luque, Enrique (2015): Modern accumulation rates and sources of organic carbon in the NE Gulf of Cádiz (SW Iberian Peninsula). Journal of Radioanalytical and Nuclear Chemistry, 305(2), 429-437, https://doi.org/10.1007/s10967-015-3991-y https://doi.pangaea.de/10.1594/PANGAEA.918394 https://doi.org/10.1594/PANGAEA.918394 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.918394 https://doi.org/10.1007/s10967-015-3991-y |
_version_ |
1766138680654692352 |