Data set: Chronostratigraphic, Sedimentological and Geochemical Data

Data set: Chronostratigraphic, Sedimentological and Geochemical Data

The age-depth model for core 7 is based on four radiocarbon (14C) dates from well-preserved monospecific samples of planktonic foraminifera (Neogloboquadrina incompta or Globorotalia inflata) measured by accelerator mass spectrometry (AMS) at the Poznan Radiocarbon Laboratory (https://radiocarbon.pl/). Grain-size analysis and distribution were performed using a Coulter LS 100 laser particle size analyser on both the bulk fraction (223 samples) and noncarbonate fraction (465 samples) (http://www.ccit.ub.edu/EN/m6sm2.html). Grain-size statistical parameters were calculated using GRADISTAT software. Geochemical analysis was performed along core 7 with an Avaatech X-ray fluorescence (XRF) core scanner operated at both 10 kV and 30 kV and with a 1 cm sampling interval at Barcelona University (https://www.ub.edu/portal/web/dp-dinamica-terra-ocea/xrf-core-scanner-laboratory).

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Bibliographic Details
Main Authors: Alonso, Belén, Ercilla, Gemma, Ausín, Blanca
Other Authors: Ministerio de Ciencia e Innovación (España)
Format: dataset biblioteca
Language:English
Published: CSIC - Instituto de Ciencias del Mar (ICM) 2023-05-01
Subjects:Marine sediments, Chronostratigraphy, Sedimentology, Geochemical data,
Online Access:http://hdl.handle.net/10261/334516
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id dig-icm-es-10261-334516
record_format koha
institution ICM ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-icm-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del ICM España
language English
topic Marine sediments
Chronostratigraphy
Sedimentology
Geochemical data
Marine sediments
Chronostratigraphy
Sedimentology
Geochemical data
spellingShingle Marine sediments
Chronostratigraphy
Sedimentology
Geochemical data
Marine sediments
Chronostratigraphy
Sedimentology
Geochemical data
Alonso, Belén
Ercilla, Gemma
Ausín, Blanca
Data set: Chronostratigraphic, Sedimentological and Geochemical Data
description The age-depth model for core 7 is based on four radiocarbon (14C) dates from well-preserved monospecific samples of planktonic foraminifera (Neogloboquadrina incompta or Globorotalia inflata) measured by accelerator mass spectrometry (AMS) at the Poznan Radiocarbon Laboratory (https://radiocarbon.pl/). Grain-size analysis and distribution were performed using a Coulter LS 100 laser particle size analyser on both the bulk fraction (223 samples) and noncarbonate fraction (465 samples) (http://www.ccit.ub.edu/EN/m6sm2.html). Grain-size statistical parameters were calculated using GRADISTAT software. Geochemical analysis was performed along core 7 with an Avaatech X-ray fluorescence (XRF) core scanner operated at both 10 kV and 30 kV and with a 1 cm sampling interval at Barcelona University (https://www.ub.edu/portal/web/dp-dinamica-terra-ocea/xrf-core-scanner-laboratory).
author2 Ministerio de Ciencia e Innovación (España)
author_facet Ministerio de Ciencia e Innovación (España)
Alonso, Belén
Ercilla, Gemma
Ausín, Blanca
format dataset
topic_facet Marine sediments
Chronostratigraphy
Sedimentology
Geochemical data
author Alonso, Belén
Ercilla, Gemma
Ausín, Blanca
author_sort Alonso, Belén
title Data set: Chronostratigraphic, Sedimentological and Geochemical Data
title_short Data set: Chronostratigraphic, Sedimentological and Geochemical Data
title_full Data set: Chronostratigraphic, Sedimentological and Geochemical Data
title_fullStr Data set: Chronostratigraphic, Sedimentological and Geochemical Data
title_full_unstemmed Data set: Chronostratigraphic, Sedimentological and Geochemical Data
title_sort data set: chronostratigraphic, sedimentological and geochemical data
publisher CSIC - Instituto de Ciencias del Mar (ICM)
publishDate 2023-05-01
url http://hdl.handle.net/10261/334516
work_keys_str_mv AT alonsobelen datasetchronostratigraphicsedimentologicalandgeochemicaldata
AT ercillagemma datasetchronostratigraphicsedimentologicalandgeochemicaldata
AT ausinblanca datasetchronostratigraphicsedimentologicalandgeochemicaldata
_version_ 1777668044348194816
spelling dig-icm-es-10261-3345162023-09-05T09:31:28Z Data set: Chronostratigraphic, Sedimentological and Geochemical Data Alonso, Belén Ercilla, Gemma Ausín, Blanca Ministerio de Ciencia e Innovación (España) Ministerio de Economía y Competitividad (España) Alonso, Belén [0000-0002-3138-5260] Ercilla, Gemma [0000-0002-9709-2938] Ercilla, Gemma Alonso, Belén; Ercilla, Gemma Marine sediments Chronostratigraphy Sedimentology Geochemical data The age-depth model for core 7 is based on four radiocarbon (14C) dates from well-preserved monospecific samples of planktonic foraminifera (Neogloboquadrina incompta or Globorotalia inflata) measured by accelerator mass spectrometry (AMS) at the Poznan Radiocarbon Laboratory (https://radiocarbon.pl/). Grain-size analysis and distribution were performed using a Coulter LS 100 laser particle size analyser on both the bulk fraction (223 samples) and noncarbonate fraction (465 samples) (http://www.ccit.ub.edu/EN/m6sm2.html). Grain-size statistical parameters were calculated using GRADISTAT software. Geochemical analysis was performed along core 7 with an Avaatech X-ray fluorescence (XRF) core scanner operated at both 10 kV and 30 kV and with a 1 cm sampling interval at Barcelona University (https://www.ub.edu/portal/web/dp-dinamica-terra-ocea/xrf-core-scanner-laboratory). The research presents for the first time a jointly analysis about the impact of the light intermediate Mediterranean (LMW) and dense deep Mediterranean (DMW) bottom currents on the sedimentation in the Alboran Sea (SW Mediterranean) and its paleoceanographic significance in response to climatic oscillations from the last glacial period to the Holocene. For that, an integration of chronostratigraphical, sedimentological, and compositional data from contourites formed by those water masses is carried out. That integration enable us to define three distinct contourite stratigraphic models. (I) The contourite terrace model, characterized by coarse-grained contourites, which is an archive of the interplay between the high-energy Atlantic Water-LMW interface and glacioeustasy from the Younger Dryas to the Holocene. (II) The contourite drift models, which are archives of rapid ocean-climate coupled fluctuations since 29.5 kyr. They comprise coarse-grained contourites formed by a relatively fast LMW and fine-grained contourites formed by a relatively weak DMW, except for the Heinrich Stadials HS3 to HS1 and YD when coarse-grained contourites were deposited. (III) The contourite/turbidite mixed model represents another archive of DMW and glacioeustasy interplay from the end of the late Pleistocene to Holocene. That contourite stratigraphy allows us to infer for the first time the relative variability of the LMW versus DMW flow regimes, which records differences and similarities. The similarities indicate that the LMW and DMW fluctuations occur in parallel at millennial and centennial time scales. The differences refer to the overall higher velocity of LMW versus DMW; the magnitude changes in velocities that are lower for LMW and higher for DMW; the recognition of three short ventilation events (a, b, c) during HS1 and HS2 for only DMW; and the distinct LMW and DMW responses to the onset of glacial conditions and return to interglacial conditions during the HSs, YD and Holocene cold periods CONTOURIBER (Ref. CTM 2008-06399-C04); FAUCES (CTM2015-65461-C2-1-R) Tables showing the Oxygen isotope (δ18O) results of cores 7 and C8; the texture, D50, and sorting of bulk fraction from all studied cores and sand percentage, D50, and UP10 percentage of non-carbonate fraction from cores 7 and C8; and the Zr/Rb ratio of cores 7 and C8 Peer reviewed 2023-09-05T08:06:57Z 2023-09-05T08:06:57Z 2023-05-01 dataset Alonso, Belén; Ercilla, Gemma; Ausín, Blanca; 2023; "Data set: Chronostratigraphic, Sedimentological and Geochemical Data"; DIGITAL.CSIC; https://doi.org/ ; http://hdl.handle.net/10261/334516 http://hdl.handle.net/10261/334516 en #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO//CTM2015-65461-C2-1-R/ES/FACTORES DE RIESGO GEOLOGICO ASOCIADO A CABECERAS DE CAÑONES SUBMARINOS DEL SUR DE LA PENINSULA IBERICA/ Alonso, Belén; Ercilla, Gemma; Juan, Carmen; López-González, Nieves; Cacho, Isabel; Francés, Guillermo; Palomino, Desirée; Bárcenas, Patricia; Yenes, Mariano; Nespereira, José; Ausín, Blanca; Mata, Pilar; Casas, David; Contourite stratigraphic models linked to the light intermediate versus dense deep Mediterranean water flow regime variations (Alboran Sea, SW Mediterranean); Marine Geology (accepted) Microsoft Excel Sí open Excel file (.xlsx) lat=36º0’00”N-36º22’30”N; long=5º15’00”W-5º45’00”W start=2010-09-17; end=2010-10-14; start=2018-10-04; end=2018-10-31 CSIC - Instituto de Ciencias del Mar (ICM)

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