Palaeoenvironmental changes in the Iberian central system during the Late-glacial and Holocene as inferred from geochemical data: A case study of the Navamuño depression in western Spain
The Iberian Central System (ICS) is a clue region to reveal Mediterranean/Atlantic inferences over Iberia. We present a multidisciplinary study from western Spain conducted in the Navamuño depression (ND), covering the last 16.8 ka (cal BP). A reconstruction of the palaeotemperature from the resulti...
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ftcsic:oai:digital.csic.es:10261/257628 2024-02-11T10:04:29+01:00 Palaeoenvironmental changes in the Iberian central system during the Late-glacial and Holocene as inferred from geochemical data: A case study of the Navamuño depression in western Spain Turu, Valentí Carrasco, Rosa M. López Sáez, José Antonio Pontevedra Pombal, Xabier Pedraza, Javier Luelmo Lautenschlaeger, Reyes Pérez Díaz, Sebastián Echeverria Moreno, Anna Frigola, Jaime Alba Sánchez, Fracisca Sánchez Vizcaíno, Jesús Pèlachs Mañosa, Albert Cunill Artigas, Raquel Nadal Tersa, Jordi Mur Cacuho, Elena Soriano López, Juan Manuel Ministerio de Ciencia, Innovación y Universidades (España) López Sáez, José Antonio Pontevedra Pombal, Xabier 2021 http://hdl.handle.net/10261/257628 en eng Elsevier #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020MICIU/ICTI2017‐2020/CGL2016-78380-P info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020MICIU/ICTI2017‐2020/PID2020-117685 GB-I00 info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020MICIU/ICTI2017‐2020/RTI2018-101714-B-I00 Publisher's version https://doi.org/10.1016/j.catena.2021.105689 Sí Catena, Volume 207, December 2021, 105689 0341-8162 http://hdl.handle.net/10261/257628 open Late Glacial Holocene Geochemistry Palaeoclimate Dust-Ashs-Aerosols artículo http://purl.org/coar/resource_type/c_6501 2021 ftcsic https://doi.org/10.1016/j.catena.2021.105689 2024-01-16T11:17:18Z The Iberian Central System (ICS) is a clue region to reveal Mediterranean/Atlantic inferences over Iberia. We present a multidisciplinary study from western Spain conducted in the Navamuño depression (ND), covering the last 16.8 ka (cal BP). A reconstruction of the palaeotemperature from the resulting geochemical data highlights four cold and dry intervals, namely, the Oldest Dryas, Older Dryas, Intra-Allerød Cold Period (IACP), and the Younger Dryas, along with warmer intervals: the Bølling (14.7–14 ka) and the Allerød (12.9–12.6 ka); however, the Greenland Interstadial GI-1c (13.4–13.1 ka) is barely distinguishable in the ND. Despite the shortage of biomass to sustain fire, the earliest charcoals are from ~14.4–13.8 ka. Evidence of ash/dust events overprinting the geochemical background starts at ~13.8–12.8 ka. Significant fire activity in the Early Holocene at ~11.7–10.6 ka affected the ND, matching the westernmost ICS data. This period includes short oceanic spells inferred from Cl peaks at ~10.9–10.2 ka and three cold intervals at 11.4, 9.3, and 8.2 ka disrupted the progressive temperature increase. The Mid-Holocene showed a continuously increasing trend towards an arid climate, peaking at 4.2 ka under a pervasive dust influx from North Africa, which has prevailed since almost ~7.9 ka. A prominent volcanic event at ~6.8–5.8 ka is in Navamuño and Roñanzas (Asturias, N Spain; Gallego et al., 2013) identified from heavy metal-rich layer, synchronous with the last known eruption of the Calatrava volcanic field (South-Central Spain; Poblete-Piedrabuena et al., 2019). This volcanic eruption could affect many other regions half north of Iberia. The pervasive presence of oceanic aerosols in the last three millennia (2.8 ka ~ ) allowed the formation of a Cl-rich peat layer during the Ibero-Roman humid period ~2.1 ka, before a changing around ~0.4 ka toward colder and drier conditions at the Little Ice Age (LIA) period. This study was funded by the LATESICE-CGL2016-78380-P, FINICES- PID2020-117685 GB-I00 and ... Article in Journal/Newspaper Greenland Digital.CSIC (Spanish National Research Council) Greenland Poblete ENVELOPE(-62.350,-62.350,-64.667,-64.667) CATENA 207 105689 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
Late Glacial Holocene Geochemistry Palaeoclimate Dust-Ashs-Aerosols |
spellingShingle |
Late Glacial Holocene Geochemistry Palaeoclimate Dust-Ashs-Aerosols Turu, Valentí Carrasco, Rosa M. López Sáez, José Antonio Pontevedra Pombal, Xabier Pedraza, Javier Luelmo Lautenschlaeger, Reyes Pérez Díaz, Sebastián Echeverria Moreno, Anna Frigola, Jaime Alba Sánchez, Fracisca Sánchez Vizcaíno, Jesús Pèlachs Mañosa, Albert Cunill Artigas, Raquel Nadal Tersa, Jordi Mur Cacuho, Elena Soriano López, Juan Manuel Palaeoenvironmental changes in the Iberian central system during the Late-glacial and Holocene as inferred from geochemical data: A case study of the Navamuño depression in western Spain |
topic_facet |
Late Glacial Holocene Geochemistry Palaeoclimate Dust-Ashs-Aerosols |
description |
The Iberian Central System (ICS) is a clue region to reveal Mediterranean/Atlantic inferences over Iberia. We present a multidisciplinary study from western Spain conducted in the Navamuño depression (ND), covering the last 16.8 ka (cal BP). A reconstruction of the palaeotemperature from the resulting geochemical data highlights four cold and dry intervals, namely, the Oldest Dryas, Older Dryas, Intra-Allerød Cold Period (IACP), and the Younger Dryas, along with warmer intervals: the Bølling (14.7–14 ka) and the Allerød (12.9–12.6 ka); however, the Greenland Interstadial GI-1c (13.4–13.1 ka) is barely distinguishable in the ND. Despite the shortage of biomass to sustain fire, the earliest charcoals are from ~14.4–13.8 ka. Evidence of ash/dust events overprinting the geochemical background starts at ~13.8–12.8 ka. Significant fire activity in the Early Holocene at ~11.7–10.6 ka affected the ND, matching the westernmost ICS data. This period includes short oceanic spells inferred from Cl peaks at ~10.9–10.2 ka and three cold intervals at 11.4, 9.3, and 8.2 ka disrupted the progressive temperature increase. The Mid-Holocene showed a continuously increasing trend towards an arid climate, peaking at 4.2 ka under a pervasive dust influx from North Africa, which has prevailed since almost ~7.9 ka. A prominent volcanic event at ~6.8–5.8 ka is in Navamuño and Roñanzas (Asturias, N Spain; Gallego et al., 2013) identified from heavy metal-rich layer, synchronous with the last known eruption of the Calatrava volcanic field (South-Central Spain; Poblete-Piedrabuena et al., 2019). This volcanic eruption could affect many other regions half north of Iberia. The pervasive presence of oceanic aerosols in the last three millennia (2.8 ka ~ ) allowed the formation of a Cl-rich peat layer during the Ibero-Roman humid period ~2.1 ka, before a changing around ~0.4 ka toward colder and drier conditions at the Little Ice Age (LIA) period. This study was funded by the LATESICE-CGL2016-78380-P, FINICES- PID2020-117685 GB-I00 and ... |
author2 |
Ministerio de Ciencia, Innovación y Universidades (España) López Sáez, José Antonio Pontevedra Pombal, Xabier |
format |
Article in Journal/Newspaper |
author |
Turu, Valentí Carrasco, Rosa M. López Sáez, José Antonio Pontevedra Pombal, Xabier Pedraza, Javier Luelmo Lautenschlaeger, Reyes Pérez Díaz, Sebastián Echeverria Moreno, Anna Frigola, Jaime Alba Sánchez, Fracisca Sánchez Vizcaíno, Jesús Pèlachs Mañosa, Albert Cunill Artigas, Raquel Nadal Tersa, Jordi Mur Cacuho, Elena Soriano López, Juan Manuel |
author_facet |
Turu, Valentí Carrasco, Rosa M. López Sáez, José Antonio Pontevedra Pombal, Xabier Pedraza, Javier Luelmo Lautenschlaeger, Reyes Pérez Díaz, Sebastián Echeverria Moreno, Anna Frigola, Jaime Alba Sánchez, Fracisca Sánchez Vizcaíno, Jesús Pèlachs Mañosa, Albert Cunill Artigas, Raquel Nadal Tersa, Jordi Mur Cacuho, Elena Soriano López, Juan Manuel |
author_sort |
Turu, Valentí |
title |
Palaeoenvironmental changes in the Iberian central system during the Late-glacial and Holocene as inferred from geochemical data: A case study of the Navamuño depression in western Spain |
title_short |
Palaeoenvironmental changes in the Iberian central system during the Late-glacial and Holocene as inferred from geochemical data: A case study of the Navamuño depression in western Spain |
title_full |
Palaeoenvironmental changes in the Iberian central system during the Late-glacial and Holocene as inferred from geochemical data: A case study of the Navamuño depression in western Spain |
title_fullStr |
Palaeoenvironmental changes in the Iberian central system during the Late-glacial and Holocene as inferred from geochemical data: A case study of the Navamuño depression in western Spain |
title_full_unstemmed |
Palaeoenvironmental changes in the Iberian central system during the Late-glacial and Holocene as inferred from geochemical data: A case study of the Navamuño depression in western Spain |
title_sort |
palaeoenvironmental changes in the iberian central system during the late-glacial and holocene as inferred from geochemical data: a case study of the navamuño depression in western spain |
publisher |
Elsevier |
publishDate |
2021 |
url |
http://hdl.handle.net/10261/257628 |
long_lat |
ENVELOPE(-62.350,-62.350,-64.667,-64.667) |
geographic |
Greenland Poblete |
geographic_facet |
Greenland Poblete |
genre |
Greenland |
genre_facet |
Greenland |
op_relation |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020MICIU/ICTI2017‐2020/CGL2016-78380-P info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020MICIU/ICTI2017‐2020/PID2020-117685 GB-I00 info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020MICIU/ICTI2017‐2020/RTI2018-101714-B-I00 Publisher's version https://doi.org/10.1016/j.catena.2021.105689 Sí Catena, Volume 207, December 2021, 105689 0341-8162 http://hdl.handle.net/10261/257628 |
op_rights |
open |
op_doi |
https://doi.org/10.1016/j.catena.2021.105689 |
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