Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Kirsty C. Crocket"'
Autor:
Kirsty C. Crocket, Emily Hill, Richard E. Abell, Clare Johnson, Stefan F. Gary, Tim Brand, Ed C. Hathorne
Publikováno v:
Frontiers in Marine Science, Vol 5 (2018)
Seawater rare earth element (REE) concentrations are increasingly applied to reconstruct water mass histories by exploiting relative changes in the distinctive normalised patterns. However, the mechanisms by which water masses gain their patterns are
Externí odkaz:
https://doaj.org/article/1ba25ab615e14461b7a699f1c26511f8
Autor:
Rebecca L. Parker, Gavin L. Foster, Marcus Gutjahr, Paul A. Wilson, Kate L. Littler, Matthew J. Cooper, Agnes Michalik, James A. Milton, Kirsty C. Crocket, Ian Bailey
Highlights • We present LGC record of the Pb isotope composition Labrador Sea seawater. • These data can be used to track Laurentide Ice Sheet extent over Hudson Bay. • LIS retreat during the PGM was relatively fast compared to the LGM • The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a88589d3d5200c23efd519da0384f996
https://eprints.soton.ac.uk/457733/
https://eprints.soton.ac.uk/457733/
Publikováno v:
Proc Natl Acad Sci U S A
The Southern Ocean is a key region for the overturning and mixing of water masses within the global ocean circulation system. Because Southern Ocean dynamics are influenced by the Southern Hemisphere westerly winds (SWW), changes in the westerly wind
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3e0b9bc4ad17587c288e6eaea8ff9919
http://hdl.handle.net/10044/1/76625
http://hdl.handle.net/10044/1/76625
Autor:
Chris D. Clark, Steve Moreton, Kirsty C. Crocket, S. Louise Callard, Derek Fabel, John A. Howe, G. M. Nowell, Sara Benetti, Riccardo Arosio
Publikováno v:
Elsevier, pp. 81-98
Marine Geology (0025-3227) (Elsevier Science Bv), 2018-08, Vol. 402, P. 81-98
Marine Geology (0025-3227) (Elsevier Science Bv), 2018-08, Vol. 402, P. 81-98
The reconstruction of past ice sheet dynamics can shed a light on long-term ice stream activity, and in turn provide constraints on the response of modern ice sheets to climate change. The Hebrides Ice Stream (HIS) flowed across part of the western S
Publikováno v:
Geochimica et Cosmochimica Acta, 265
Chemical weathering of silicate rock is one of the major long-term sinks of atmospheric CO2. While several radiogenic isotope systems (e.g. Nd, Pb, Os) in the authigenic component of marine sediments show temporal patterns that could be interpreted i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8807df1b1733b9b52cde959365a7efa9
https://hdl.handle.net/20.500.11850/365673
https://hdl.handle.net/20.500.11850/365673
Autor:
Tina van de Flierdt, Jess F. Adkins, S.K.V. Hines, Laura F. Robinson, Maureen E. Auro, Katharina Kreissig, Louisa I Bradtmiller, Myriam Lambelet, Barry J. Coles, Kirsty C. Crocket, Torben Struve
Publikováno v:
Geochemistry, Geophysics, Geosystems. 17:232-240
Isotopes of the actinide elements protactinium (Pa), thorium (Th), and uranium (U), and the lanthanide element neodymium (Nd) are often used as complementary tracers of modern and past oceanic processes. The extraction of such elements from low abund
Autor:
Stefan F. Gary, Emily Jane Hill, Richard Abell, Ed C Hathorne, Tim Brand, Clare Johnson, Kirsty C. Crocket
Publikováno v:
Frontiers in Marine Science, Vol 5 (2018)
Frontiers in Marine Science, 5 . Art.Nr. 147.
Frontiers in Marine Science
Frontiers in Marine Science, 5 . Art.Nr. 147.
Frontiers in Marine Science
Seawater rare earth element (REE) concentrations are increasingly applied to reconstruct water mass histories by exploiting relative changes in the distinctive normalised patterns. However, the mechanisms by which water masses gain their patterns are
Publikováno v:
Paleoceanography. 29:1072-1093
The last deglaciation was characterised by a series of millennial scale climate events that have been linked to deep ocean variability. While often implied in interpretations, few direct constraints exist on circulation changes at mid-depths. Here we
Publikováno v:
Chemical Geology
Precise and accurate measurements of Nd concentrations and isotopic compositions of small sample masses (≤ 30 ng Nd) are increasingly necessary in the geosciences. Here, we present a combined chemical separation and TIMS (thermal ionisation mass sp
Publikováno v:
Crocket, K, Foster, G, Vance, D, Richards, D & Tranter, M 2013, ' A Pb isotope tracer of ocean-ice sheet interaction: the record from the NE Atlantic during the Last Glacial/Interglacial cycle ', Quaternary Science Reviews, vol. 82, pp. 133-144 . https://doi.org/10.1016/j.quascirev.2013.10.020
Ice sheet-ocean interactions are both a response to climate forcing and a source of climate feedback, releasing freshwater to the surface ocean and influencing climate and atmospheric CO2 through changes in ocean circulation. Documenting the outcomes