RV SONNE SO240, Cruise Report / Fahrtbericht, Manzanillo (Mexico): May 3rd, 2015, Manzanillo (Mexico): June 16th, 2015

The research cruise SO-240 took place from May 3rd, 2015 until June 16th, 2015 at about 12°N and 118°W, approximately 900 nm offshore Mexico in the equatorial NE Pacific. This cruise started and ended in the port of Manzanillo on the west coast of Mexico. Scientists from the Federal Institute for Ge...

Full description

Bibliographic Details
Main Author: Kuhn, Thomas
Format: Report
Language:English
Published: Bundesanstalt für Geowissenschaften und Rohstoffe 2015
Subjects:
Online Access:https://dx.doi.org/10.2312/cr_so240
https://www.tib.eu/suchen/id/awi:d7cda0074675075b7225c1e296eb1c06fc18ac5a
id ftdatacite:10.2312/cr_so240
record_format openpolar
spelling ftdatacite:10.2312/cr_so240 2023-05-15T13:15:44+02:00 RV SONNE SO240, Cruise Report / Fahrtbericht, Manzanillo (Mexico): May 3rd, 2015, Manzanillo (Mexico): June 16th, 2015 Kuhn, Thomas 2015 application/pdf https://dx.doi.org/10.2312/cr_so240 https://www.tib.eu/suchen/id/awi:d7cda0074675075b7225c1e296eb1c06fc18ac5a en eng Bundesanstalt für Geowissenschaften und Rohstoffe Bundesanstalt für Geowissenschaften und Rohstoffe Earth Science Earth sciences and geology Electronic Resource report Report 2015 ftdatacite https://doi.org/10.2312/cr_so240 2022-03-10T13:06:06Z The research cruise SO-240 took place from May 3rd, 2015 until June 16th, 2015 at about 12°N and 118°W, approximately 900 nm offshore Mexico in the equatorial NE Pacific. This cruise started and ended in the port of Manzanillo on the west coast of Mexico. Scientists from the Federal Institute for Geosciences and Natural Resources (BGR), the University of Bremen, the Jacobs University Bremen, the Alfred Wegener Institute Helmholtz Center for Polar and Marine Research (AWI), Bremerhaven, Germany (AWI), and the German Centre for Marine Biodiversity Research Wilhelmshaven participated in the cruise. The objective of this cruise was to investigate the regional pattern of seawater circulation within the basaltic seafloor underneath its sediment cover. Understanding such processes is important as hydrothermal fluids can withdraw significant amounts of heat from the oceanic lithosphere by lateral fluid flow through permeable basaltic crust having an age of up to 65 Ma. Basement outcrops in-between impermeable pelagic sediments permit recharge of oxic seawater and discharge of altered and slightly heated seawater. As the seawater migrates through the basaltic crust, it mines heat from the lithosphere, starts reacting with the basaltic rocks and feeds the microbial community with oxygen and nutrients. Single-channel seismic surveys, heat flow measurements, pore-water, sediment and manganese nodule sampling as well as video mapping were carried out for these investigations. Report Alfred Wegener Institute DataCite Metadata Store (German National Library of Science and Technology) Pacific
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Earth Science
Earth sciences and geology
spellingShingle Earth Science
Earth sciences and geology
Kuhn, Thomas
RV SONNE SO240, Cruise Report / Fahrtbericht, Manzanillo (Mexico): May 3rd, 2015, Manzanillo (Mexico): June 16th, 2015
topic_facet Earth Science
Earth sciences and geology
description The research cruise SO-240 took place from May 3rd, 2015 until June 16th, 2015 at about 12°N and 118°W, approximately 900 nm offshore Mexico in the equatorial NE Pacific. This cruise started and ended in the port of Manzanillo on the west coast of Mexico. Scientists from the Federal Institute for Geosciences and Natural Resources (BGR), the University of Bremen, the Jacobs University Bremen, the Alfred Wegener Institute Helmholtz Center for Polar and Marine Research (AWI), Bremerhaven, Germany (AWI), and the German Centre for Marine Biodiversity Research Wilhelmshaven participated in the cruise. The objective of this cruise was to investigate the regional pattern of seawater circulation within the basaltic seafloor underneath its sediment cover. Understanding such processes is important as hydrothermal fluids can withdraw significant amounts of heat from the oceanic lithosphere by lateral fluid flow through permeable basaltic crust having an age of up to 65 Ma. Basement outcrops in-between impermeable pelagic sediments permit recharge of oxic seawater and discharge of altered and slightly heated seawater. As the seawater migrates through the basaltic crust, it mines heat from the lithosphere, starts reacting with the basaltic rocks and feeds the microbial community with oxygen and nutrients. Single-channel seismic surveys, heat flow measurements, pore-water, sediment and manganese nodule sampling as well as video mapping were carried out for these investigations.
format Report
author Kuhn, Thomas
author_facet Kuhn, Thomas
author_sort Kuhn, Thomas
title RV SONNE SO240, Cruise Report / Fahrtbericht, Manzanillo (Mexico): May 3rd, 2015, Manzanillo (Mexico): June 16th, 2015
title_short RV SONNE SO240, Cruise Report / Fahrtbericht, Manzanillo (Mexico): May 3rd, 2015, Manzanillo (Mexico): June 16th, 2015
title_full RV SONNE SO240, Cruise Report / Fahrtbericht, Manzanillo (Mexico): May 3rd, 2015, Manzanillo (Mexico): June 16th, 2015
title_fullStr RV SONNE SO240, Cruise Report / Fahrtbericht, Manzanillo (Mexico): May 3rd, 2015, Manzanillo (Mexico): June 16th, 2015
title_full_unstemmed RV SONNE SO240, Cruise Report / Fahrtbericht, Manzanillo (Mexico): May 3rd, 2015, Manzanillo (Mexico): June 16th, 2015
title_sort rv sonne so240, cruise report / fahrtbericht, manzanillo (mexico): may 3rd, 2015, manzanillo (mexico): june 16th, 2015
publisher Bundesanstalt für Geowissenschaften und Rohstoffe
publishDate 2015
url https://dx.doi.org/10.2312/cr_so240
https://www.tib.eu/suchen/id/awi:d7cda0074675075b7225c1e296eb1c06fc18ac5a
geographic Pacific
geographic_facet Pacific
genre Alfred Wegener Institute
genre_facet Alfred Wegener Institute
op_rights Bundesanstalt für Geowissenschaften und Rohstoffe
op_doi https://doi.org/10.2312/cr_so240
_version_ 1766270758146801664