Glaucony authigenesis, maturity and alteration in the Weddell Sea: An indicator of paleoenvironmental conditions before the onset of Antarctic glaciation
Three types of glaucony grains were identified in the late Eocene (~35.5-34.1 Ma) sediments from Ocean Drilling Program (ODP) Hole 696B in the northwestern Weddell Sea (Antarctica). The grains are K2O-rich (~7 wt%) and formed by smectite-poor interstratified ~10 Å glauconite-smectite with flaky/rose...
Published in: | Scientific Reports |
---|---|
Main Authors: | , , , , , , |
Other Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Nature Publishing Group
2019
|
Subjects: | |
Online Access: | http://hdl.handle.net/10261/205258 https://doi.org/10.1038/s41598-019-50107-1 https://doi.org/10.13039/501100000780 https://doi.org/10.13039/501100004837 https://doi.org/10.13039/501100011011 |
id |
ftcsic:oai:digital.csic.es:10261/205258 |
---|---|
record_format |
openpolar |
spelling |
ftcsic:oai:digital.csic.es:10261/205258 2024-02-11T09:58:18+01:00 Glaucony authigenesis, maturity and alteration in the Weddell Sea: An indicator of paleoenvironmental conditions before the onset of Antarctic glaciation López-Quirós, Adrián Escutia, Carlota Sánchez Navas, Antonio Nieto, F. García-Casco, Antonio Martín Algarra, A. Evangelinos, Dimitris Ministerio de Ciencia e Innovación (España) European Commission Junta de Andalucía 2019-09-19 http://hdl.handle.net/10261/205258 https://doi.org/10.1038/s41598-019-50107-1 https://doi.org/10.13039/501100000780 https://doi.org/10.13039/501100004837 https://doi.org/10.13039/501100011011 unknown Nature Publishing Group #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2014-60451-C2-1-P info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/CTM2017-89711-C2-1-P info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CGL2016-75679P Publisher's version http://dx.doi.org/10.1038/s41598-019-50107-1 Sí doi:10.1038/s41598-019-50107-1 issn: 2045-2322 Scientific Reports 9: 13580 (2019) http://hdl.handle.net/10261/205258 http://dx.doi.org/10.13039/501100000780 http://dx.doi.org/10.13039/501100004837 http://dx.doi.org/10.13039/501100011011 31537907 open artículo http://purl.org/coar/resource_type/c_6501 2019 ftcsic https://doi.org/10.1038/s41598-019-50107-110.13039/50110000078010.13039/50110000483710.13039/501100011011 2024-01-16T10:50:46Z Three types of glaucony grains were identified in the late Eocene (~35.5-34.1 Ma) sediments from Ocean Drilling Program (ODP) Hole 696B in the northwestern Weddell Sea (Antarctica). The grains are K2O-rich (~7 wt%) and formed by smectite-poor interstratified ~10 Å glauconite-smectite with flaky/rosette-shaped surface nanostructures. Two glaucony types reflect an evolved (types 1 and 2 glaucony; less mature to mature) stage and long term glauconitization, attesting to the glaucony grains being formed in situ, whereas the third type (type 3 glaucony) shows evidences of alteration and reworking from nearby areas. Conditions for the glaucony authigenesis occurred in an open-shelf environment deeper than 50 m, under sub-oxic conditions near the sediment-water interface. These environmental conditions were triggered by low sedimentation rates and recurrent winnowing action by bottom-currents, leading to stratigraphic condensation. The condensed glaucony-bearing section provides an overview of continuous sea-level rise conditions pre-dating the onset of Antarctic glaciation during the Eocene-Oligocene transition. Sediment burial, drop of O2 levels, and ongoing reducing (postoxic to sulphidic) conditions at Hole 696B, resulting in iron-sulphide precipitation, were a key limiting factor for the glauconitization by sequestration of Fe2+. This research used samples from the ODP. We thank the staff at the Gulf Coast core repository for assistance in ODP Leg 113 core handling and shipping. Funding for this research is provided by the Spanish Ministry of Science and Innovation (grants CTM2014-60451-C2-1-P and CTM2017-89711-C2-1-P, CGL2016-75679P) co-funded by the European Union through FEDER funds and RNM-208 group (Discontinuidades estratigráficas, Junta de Andalucía, Spain). We acknowledge the help of Dr. María del Mar Abad, Dr. Isabel Sánchez Almazo, Dr. Miguel Angel Hidalgo, Dr. Miguel Angel Salas, and Isabel Nieto (Scientific Instrumentation Center of the University of Granada, CIC) for their help along different ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Weddell Sea Digital.CSIC (Spanish National Research Council) Antarctic Salas ENVELOPE(-58.417,-58.417,-63.550,-63.550) Weddell Weddell Sea Scientific Reports 9 1 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
unknown |
description |
Three types of glaucony grains were identified in the late Eocene (~35.5-34.1 Ma) sediments from Ocean Drilling Program (ODP) Hole 696B in the northwestern Weddell Sea (Antarctica). The grains are K2O-rich (~7 wt%) and formed by smectite-poor interstratified ~10 Å glauconite-smectite with flaky/rosette-shaped surface nanostructures. Two glaucony types reflect an evolved (types 1 and 2 glaucony; less mature to mature) stage and long term glauconitization, attesting to the glaucony grains being formed in situ, whereas the third type (type 3 glaucony) shows evidences of alteration and reworking from nearby areas. Conditions for the glaucony authigenesis occurred in an open-shelf environment deeper than 50 m, under sub-oxic conditions near the sediment-water interface. These environmental conditions were triggered by low sedimentation rates and recurrent winnowing action by bottom-currents, leading to stratigraphic condensation. The condensed glaucony-bearing section provides an overview of continuous sea-level rise conditions pre-dating the onset of Antarctic glaciation during the Eocene-Oligocene transition. Sediment burial, drop of O2 levels, and ongoing reducing (postoxic to sulphidic) conditions at Hole 696B, resulting in iron-sulphide precipitation, were a key limiting factor for the glauconitization by sequestration of Fe2+. This research used samples from the ODP. We thank the staff at the Gulf Coast core repository for assistance in ODP Leg 113 core handling and shipping. Funding for this research is provided by the Spanish Ministry of Science and Innovation (grants CTM2014-60451-C2-1-P and CTM2017-89711-C2-1-P, CGL2016-75679P) co-funded by the European Union through FEDER funds and RNM-208 group (Discontinuidades estratigráficas, Junta de Andalucía, Spain). We acknowledge the help of Dr. María del Mar Abad, Dr. Isabel Sánchez Almazo, Dr. Miguel Angel Hidalgo, Dr. Miguel Angel Salas, and Isabel Nieto (Scientific Instrumentation Center of the University of Granada, CIC) for their help along different ... |
author2 |
Ministerio de Ciencia e Innovación (España) European Commission Junta de Andalucía |
format |
Article in Journal/Newspaper |
author |
López-Quirós, Adrián Escutia, Carlota Sánchez Navas, Antonio Nieto, F. García-Casco, Antonio Martín Algarra, A. Evangelinos, Dimitris |
spellingShingle |
López-Quirós, Adrián Escutia, Carlota Sánchez Navas, Antonio Nieto, F. García-Casco, Antonio Martín Algarra, A. Evangelinos, Dimitris Glaucony authigenesis, maturity and alteration in the Weddell Sea: An indicator of paleoenvironmental conditions before the onset of Antarctic glaciation |
author_facet |
López-Quirós, Adrián Escutia, Carlota Sánchez Navas, Antonio Nieto, F. García-Casco, Antonio Martín Algarra, A. Evangelinos, Dimitris |
author_sort |
López-Quirós, Adrián |
title |
Glaucony authigenesis, maturity and alteration in the Weddell Sea: An indicator of paleoenvironmental conditions before the onset of Antarctic glaciation |
title_short |
Glaucony authigenesis, maturity and alteration in the Weddell Sea: An indicator of paleoenvironmental conditions before the onset of Antarctic glaciation |
title_full |
Glaucony authigenesis, maturity and alteration in the Weddell Sea: An indicator of paleoenvironmental conditions before the onset of Antarctic glaciation |
title_fullStr |
Glaucony authigenesis, maturity and alteration in the Weddell Sea: An indicator of paleoenvironmental conditions before the onset of Antarctic glaciation |
title_full_unstemmed |
Glaucony authigenesis, maturity and alteration in the Weddell Sea: An indicator of paleoenvironmental conditions before the onset of Antarctic glaciation |
title_sort |
glaucony authigenesis, maturity and alteration in the weddell sea: an indicator of paleoenvironmental conditions before the onset of antarctic glaciation |
publisher |
Nature Publishing Group |
publishDate |
2019 |
url |
http://hdl.handle.net/10261/205258 https://doi.org/10.1038/s41598-019-50107-1 https://doi.org/10.13039/501100000780 https://doi.org/10.13039/501100004837 https://doi.org/10.13039/501100011011 |
long_lat |
ENVELOPE(-58.417,-58.417,-63.550,-63.550) |
geographic |
Antarctic Salas Weddell Weddell Sea |
geographic_facet |
Antarctic Salas Weddell Weddell Sea |
genre |
Antarc* Antarctic Antarctica Weddell Sea |
genre_facet |
Antarc* Antarctic Antarctica Weddell Sea |
op_relation |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2014-60451-C2-1-P info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/CTM2017-89711-C2-1-P info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CGL2016-75679P Publisher's version http://dx.doi.org/10.1038/s41598-019-50107-1 Sí doi:10.1038/s41598-019-50107-1 issn: 2045-2322 Scientific Reports 9: 13580 (2019) http://hdl.handle.net/10261/205258 http://dx.doi.org/10.13039/501100000780 http://dx.doi.org/10.13039/501100004837 http://dx.doi.org/10.13039/501100011011 31537907 |
op_rights |
open |
op_doi |
https://doi.org/10.1038/s41598-019-50107-110.13039/50110000078010.13039/50110000483710.13039/501100011011 |
container_title |
Scientific Reports |
container_volume |
9 |
container_issue |
1 |
_version_ |
1790593913922256896 |