Recent morpho-sedimentary processes in Dove Basin, southern Scotia Sea, Antarctica: A basin-scale case of interaction between bottom currents and mass movements

F. J. Lobo; A. López-Quirós; F. J. Hernández-Molina; L. F. Pérez; M. García; D. Evangelinos; F. Bohoyo; J. Rodríguez-Fernández; A. Salabarnada; A. Maldonado

doi:10.1016/j.margeo.2021.106598

Recent morpho-sedimentary processes in Dove Basin, southern Scotia Sea, Antarctica: A basin-scale case of interaction between bottom currents and mass movements

F. J. Lobo, A. López-Quirós, F. J. Hernández-Molina, L. F. Pérez, M. García, D. Evangelinos, F. Bohoyo, J. Rodríguez-Fernández, A. Salabarnada, A. Maldonado

Research output: Contribution to journal › Article › peer-review

Original language	English
Article number	106598
Journal	Marine Geology
Volume	441
Early online date	11 Aug 2021
DOIs	https://doi.org/10.1016/j.margeo.2021.106598
Publication status	E-pub ahead of print - 11 Aug 2021

Keywords

Antarctic Circumpolar Current
Contourites
Dove Basin
Gravity flows
Scotia Sea
Sub-bottom stratigraphy
Weddell Sea Deep Water

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10.1016/j.margeo.2021.106598Licence: CC BY

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Lobo, F. J., López-Quirós, A., Hernández-Molina, F. J., Pérez, L. F., García, M., Evangelinos, D., Bohoyo, F., Rodríguez-Fernández, J., Salabarnada, A., & Maldonado, A. (2021). Recent morpho-sedimentary processes in Dove Basin, southern Scotia Sea, Antarctica: A basin-scale case of interaction between bottom currents and mass movements. Marine Geology, 441, Article 106598. Advance online publication. https://doi.org/10.1016/j.margeo.2021.106598

@article{c976057f23a941689f51665a38a0d8c8,

title = "Recent morpho-sedimentary processes in Dove Basin, southern Scotia Sea, Antarctica: A basin-scale case of interaction between bottom currents and mass movements",

keywords = "Antarctic Circumpolar Current, Contourites, Dove Basin, Gravity flows, Scotia Sea, Sub-bottom stratigraphy, Weddell Sea Deep Water",

author = "Lobo, {F. J.} and A. L{\'o}pez-Quir{\'o}s and Hern{\'a}ndez-Molina, {F. J.} and P{\'e}rez, {L. F.} and M. Garc{\'i}a and D. Evangelinos and F. Bohoyo and J. Rodr{\'i}guez-Fern{\'a}ndez and A. Salabarnada and A. Maldonado",

note = "Funding Information: Funding for this research was provided by the Spanish Ministry of Science and Innovation (grants CTM2014-60451-C2-1/2-P and CTM2017-89711-C2-1/2-P) co-funded by the European Union through FEDER funds. The research was conducted in collaboration with ?The Drifters Research Group? of the Royal Holloway University of London (UK), and is also related to the projects CTM 2012-39599-C03, CGL2016-80445-R, CTM2016-75129-C3-1-R and CGL2015-74216-JIN. We thank the commander, officers and crew of the BIO HESPERIDES for their support in obtaining the data, sometimes under severe sea conditions. Jean Sanders reviewed the English style of the manuscript. Rob Larter (BAS, UK) and an anonymous reviewer provided numerous useful remarks that improved an initial version of the manuscript. Seismic interpretations were made using the IHS Kingdom? software, thanks to the participation of the Instituto Andaluz de Ciencias de la Tierra in the IHS University Grant program. Funding Information: Funding for this research was provided by the Spanish Ministry of Science and Innovation (grants CTM2014-60451-C2-1/2-P and CTM2017-89711-C2-1/2-P ) co-funded by the European Union through FEDER funds. The research was conducted in collaboration with {\textquoteleft}The Drifters Research Group{\textquoteright} of the Royal Holloway University of London (UK), and is also related to the projects CTM 2012-39599-C03, CGL2016-80445-R, CTM2016-75129-C3-1-R and CGL2015-74216-JIN. We thank the commander, officers and crew of the BIO HESPERIDES for their support in obtaining the data, sometimes under severe sea conditions. Jean Sanders reviewed the English style of the manuscript. Rob Larter (BAS, UK) and an anonymous reviewer provided numerous useful remarks that improved an initial version of the manuscript. Seismic interpretations were made using the IHS Kingdom{\texttrademark} software, thanks to the participation of the Instituto Andaluz de Ciencias de la Tierra in the IHS University Grant program. Publisher Copyright: {\textcopyright} 2021 The Authors",

year = "2021",

month = aug,

day = "11",

doi = "10.1016/j.margeo.2021.106598",

language = "English",

volume = "441",

journal = "Marine Geology",

issn = "0025-3227",

publisher = "Elsevier",

}

Lobo, FJ, López-Quirós, A, Hernández-Molina, FJ, Pérez, LF, García, M, Evangelinos, D, Bohoyo, F, Rodríguez-Fernández, J, Salabarnada, A & Maldonado, A 2021, 'Recent morpho-sedimentary processes in Dove Basin, southern Scotia Sea, Antarctica: A basin-scale case of interaction between bottom currents and mass movements', Marine Geology, vol. 441, 106598. https://doi.org/10.1016/j.margeo.2021.106598

TY - JOUR

T1 - Recent morpho-sedimentary processes in Dove Basin, southern Scotia Sea, Antarctica

T2 - A basin-scale case of interaction between bottom currents and mass movements

AU - Lobo, F. J.

AU - López-Quirós, A.

AU - Hernández-Molina, F. J.

AU - Pérez, L. F.

AU - García, M.

AU - Evangelinos, D.

AU - Bohoyo, F.

AU - Rodríguez-Fernández, J.

AU - Salabarnada, A.

AU - Maldonado, A.

N1 - Funding Information: Funding for this research was provided by the Spanish Ministry of Science and Innovation (grants CTM2014-60451-C2-1/2-P and CTM2017-89711-C2-1/2-P) co-funded by the European Union through FEDER funds. The research was conducted in collaboration with ?The Drifters Research Group? of the Royal Holloway University of London (UK), and is also related to the projects CTM 2012-39599-C03, CGL2016-80445-R, CTM2016-75129-C3-1-R and CGL2015-74216-JIN. We thank the commander, officers and crew of the BIO HESPERIDES for their support in obtaining the data, sometimes under severe sea conditions. Jean Sanders reviewed the English style of the manuscript. Rob Larter (BAS, UK) and an anonymous reviewer provided numerous useful remarks that improved an initial version of the manuscript. Seismic interpretations were made using the IHS Kingdom? software, thanks to the participation of the Instituto Andaluz de Ciencias de la Tierra in the IHS University Grant program. Funding Information: Funding for this research was provided by the Spanish Ministry of Science and Innovation (grants CTM2014-60451-C2-1/2-P and CTM2017-89711-C2-1/2-P ) co-funded by the European Union through FEDER funds. The research was conducted in collaboration with ‘The Drifters Research Group’ of the Royal Holloway University of London (UK), and is also related to the projects CTM 2012-39599-C03, CGL2016-80445-R, CTM2016-75129-C3-1-R and CGL2015-74216-JIN. We thank the commander, officers and crew of the BIO HESPERIDES for their support in obtaining the data, sometimes under severe sea conditions. Jean Sanders reviewed the English style of the manuscript. Rob Larter (BAS, UK) and an anonymous reviewer provided numerous useful remarks that improved an initial version of the manuscript. Seismic interpretations were made using the IHS Kingdom™ software, thanks to the participation of the Instituto Andaluz de Ciencias de la Tierra in the IHS University Grant program. Publisher Copyright: © 2021 The Authors

PY - 2021/8/11

Y1 - 2021/8/11

KW - Antarctic Circumpolar Current

KW - Contourites

KW - Dove Basin

KW - Gravity flows

KW - Scotia Sea

KW - Sub-bottom stratigraphy

KW - Weddell Sea Deep Water

UR - http://www.scopus.com/inward/record.url?scp=85113301724&partnerID=8YFLogxK

U2 - 10.1016/j.margeo.2021.106598

DO - 10.1016/j.margeo.2021.106598

M3 - Article

AN - SCOPUS:85113301724

SN - 0025-3227

VL - 441

JO - Marine Geology

JF - Marine Geology

M1 - 106598

ER -

Recent morpho-sedimentary processes in Dove Basin, southern Scotia Sea, Antarctica: A basin-scale case of interaction between bottom currents and mass movements

Keywords

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