dc.contributor.author |
Cortina, Aleix |
|
dc.contributor.author |
Filippelli, Gabriel |
|
dc.contributor.author |
Ochoa, Diana |
|
dc.contributor.author |
Javier Sierro, Francisco |
|
dc.contributor.author |
Flores, Jose-Abel |
|
dc.contributor.author |
Grimalt, Joan O. |
|
dc.date.accessioned |
2018-11-30T23:41:32Z |
|
dc.date.available |
2018-11-30T23:41:32Z |
|
dc.date.issued |
2018 |
|
dc.identifier.uri |
https://hdl.handle.net/20.500.12866/4224 |
|
dc.description.abstract |
The burial of phosphorus (P) in continental margin sediments is a critical component of the marine reactive P budget, and thus an important factor in marine biological productivity. We determined downcore records of P from a site drilled on the upper slope of the Gulf of Lions (PRGL 1), northwestern Mediterranean Sea. Changes in total P content were monitored from Marine Isotope Stage (MIS) 6 to MIS 11. In addition, in two selected intervals (248-277 ka and 306-342 ka) the total P record was expanded by adding detailed geochemical analyses of the various P fractions, including oxyhydroxide-associated P, authigenic P, detrital P and organic P. Increased sedimentation rates during glacials owing to seaward migration of the Rhone's mouth, enhanced the burial of reactive P (oxyhydroxide-associated + authigenic + organic) phases by decreasing its time at the reactive sediment/water interface, in turn resulting in increasing proportion of authigenic to detrital phosphorus. The inverse was found for interglacial stages. The effects of glacial/interglacial variation in sedimentation rate over P geochemistry resulted in changes in sediment-water interface oxygenation, as well as in the efficiency of P burial, as shown by (C:P)(org) and C-org:P-react proxies respectively. Two events of high P deposition associated with authigenic (P-aut1) formation, at 335 (P-aut2) and 275 ka (P0052), were associated with periods of rapid disintegration of North Atlantic ice sheets leading to Ice Rafted Debris (IRD) deposition. These high P deposition events appear to be linked to short warm periods that followed cold episodes. Enhanced continental runoff owing to more humid conditions during short warm episodes could play a critical role for enhanced biogenic productivity and posterior authigenic P accumulation. |
en_US |
dc.language.iso |
eng |
|
dc.publisher |
Elsevier |
|
dc.relation.ispartofseries |
Palaeogeography, Palaeoclimatology, Palaeoecology |
|
dc.rights |
info:eu-repo/semantics/restrictedAccess |
|
dc.rights.uri |
https://creativecommons.org/licenses/by-nc-nd/4.0/deed.es |
|
dc.subject |
biogeochemistry |
en_US |
dc.subject |
biological production |
en_US |
dc.subject |
burial (geology) |
en_US |
dc.subject |
climate variation |
en_US |
dc.subject |
continental margin |
en_US |
dc.subject |
Gulf of Lion |
en_US |
dc.subject |
Gulf of lions |
en_US |
dc.subject |
marine isotope stage |
en_US |
dc.subject |
Mediterranean Sea |
en_US |
dc.subject |
Mediterranean Sea (Northwest) |
en_US |
dc.subject |
MIS 8 |
en_US |
dc.subject |
oxygenation |
en_US |
dc.subject |
paleoproductivity |
en_US |
dc.subject |
Paleoredox |
en_US |
dc.subject |
phosphorus |
en_US |
dc.subject |
Phosphorus paleoproductivity |
en_US |
dc.subject |
redox conditions |
en_US |
dc.subject |
sediment-water interface |
en_US |
dc.subject |
sedimentation rate |
en_US |
dc.subject |
Termination IV |
en_US |
dc.title |
Climate-driven changes in sedimentation rate influence phosphorus burial along continental margins of the northwestern Mediterranean |
en_US |
dc.type |
info:eu-repo/semantics/article |
|
dc.identifier.doi |
https://doi.org/10.1016/j.palaeo.2018.03.010 |
|
dc.subject.ocde |
https://purl.org/pe-repo/ocde/ford#1.05.03 |
|
dc.subject.ocde |
https://purl.org/pe-repo/ocde/ford#1.05.11 |
|
dc.relation.issn |
1872-616X |
|