FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2052690206> ?p ?o ?g. }

• W2052690206 endingPage "228" @default.
• W2052690206 startingPage "217" @default.
• W2052690206 abstract "The circulation patterns of the deep glacial Pacific Ocean are still debated. Difficulties arise due to the scarcity of reliable paleoceanographic records that can document the past movements and properties of Pacific Ocean water masses. Here, we jointly use delta(13)C and delta(18)O measured on the epibenthic foraminifer Cibicidoides wuellerstorfi, from the MD02-2529 sediment core collected at 1619 m water depth in the eastern equatorial Pacific, to monitor changes in water mass circulation spanning the past 150 kyr BP. After the extraction of short-term (centennial to millennial-scale) delta(13)C and delta(18)O changes, which were similar to 1.0 and 0.5 parts per thousand, respectively, we observed that these rapid delta(13)C and 8180 shifts were closely interrelated during the last 150 kyr BP. A comparison of MD02-2529 with other benthic delta(13)C records localized to the north and south of the core location revealed that MD02-2529 was alternately bathed by a northern nutrient-rich and a southern nutrient-poor water mass. The comparison provided a diagnostic for the latitudinal movements of a sharp water mass front that was particularly evident during marine isotope stages 4 and 3 on the millennial timescale. By considering that delta(13)C is an indicator of the northern vs. southern origin of the water that bathed the MD02-2529 coring site in the past, we found that a North Pacific water mass, that occasionally spreads to the eastern Pacific Ocean as deep as 1600 m and as far south as 8 degrees N, was responsible for shifts toward the positive delta(18)O we observed in the past. We then used the delta(13)C/delta(18)O relationship to reconstruct latitudinal temperature and/or salinity gradients of the water mass that were linked to changes in the northern and/or the southern water mass end-members. Evolution of the delta(13)C/delta(18)O relationship spanning the past 150 kyr BP has shed light on how hydrological processes occurring at northern and southern high latitudes are transmitted to the ocean's interior through water mass advection. (C) 2010 Elsevier B.V. All rights reserved." @default.
• W2052690206 created "2016-06-24" @default.
• W2052690206 creator A5024631008 @default.
• W2052690206 creator A5052775828 @default.
• W2052690206 creator A5059602597 @default.
• W2052690206 creator A5080323857 @default.
• W2052690206 date "2010-09-01" @default.
• W2052690206 modified "2023-10-18" @default.
• W2052690206 title "Changes in Eastern Pacific ocean ventilation at intermediate depth over the last 150 kyr BP" @default.
• W2052690206 cites W1489155911 @default.
• W2052690206 cites W1528433787 @default.
• W2052690206 cites W1562571324 @default.
• W2052690206 cites W1610113429 @default.
• W2052690206 cites W1770994388 @default.
• W2052690206 cites W1860039907 @default.
• W2052690206 cites W1882241828 @default.
• W2052690206 cites W1893787057 @default.
• W2052690206 cites W1909880476 @default.
• W2052690206 cites W1959186330 @default.
• W2052690206 cites W1969741190 @default.
• W2052690206 cites W1972925337 @default.
• W2052690206 cites W1974537329 @default.
• W2052690206 cites W1975498061 @default.
• W2052690206 cites W1976720760 @default.
• W2052690206 cites W1977740449 @default.
• W2052690206 cites W1982701446 @default.
• W2052690206 cites W1999090249 @default.
• W2052690206 cites W2000766006 @default.
• W2052690206 cites W2006481043 @default.
• W2052690206 cites W2013043138 @default.
• W2052690206 cites W2014990620 @default.
• W2052690206 cites W2016417261 @default.
• W2052690206 cites W2018424764 @default.
• W2052690206 cites W2020642721 @default.
• W2052690206 cites W2030056829 @default.
• W2052690206 cites W2037073783 @default.
• W2052690206 cites W2039566285 @default.
• W2052690206 cites W2039667302 @default.
• W2052690206 cites W2048050280 @default.
• W2052690206 cites W2048414881 @default.
• W2052690206 cites W2050469687 @default.
• W2052690206 cites W2051226623 @default.
• W2052690206 cites W2054054760 @default.
• W2052690206 cites W2055015335 @default.
• W2052690206 cites W2058931034 @default.
• W2052690206 cites W2059198684 @default.
• W2052690206 cites W2063409788 @default.
• W2052690206 cites W2064368240 @default.
• W2052690206 cites W2065111040 @default.
• W2052690206 cites W2067787027 @default.
• W2052690206 cites W2068731501 @default.
• W2052690206 cites W2074482550 @default.
• W2052690206 cites W2074887696 @default.
• W2052690206 cites W2075385168 @default.
• W2052690206 cites W2081319507 @default.
• W2052690206 cites W2083072147 @default.
• W2052690206 cites W2085194150 @default.
• W2052690206 cites W2085202979 @default.
• W2052690206 cites W2087285665 @default.
• W2052690206 cites W2090767277 @default.
• W2052690206 cites W2091642911 @default.
• W2052690206 cites W2093142430 @default.
• W2052690206 cites W2093722277 @default.
• W2052690206 cites W2099667979 @default.
• W2052690206 cites W2107087656 @default.
• W2052690206 cites W2113920401 @default.
• W2052690206 cites W2117175737 @default.
• W2052690206 cites W2120668627 @default.
• W2052690206 cites W2121128303 @default.
• W2052690206 cites W2121913826 @default.
• W2052690206 cites W2123900986 @default.
• W2052690206 cites W2135254726 @default.
• W2052690206 cites W2135878067 @default.
• W2052690206 cites W2152188824 @default.
• W2052690206 cites W2152368443 @default.
• W2052690206 cites W2163819305 @default.
• W2052690206 cites W2163961280 @default.
• W2052690206 cites W2166646125 @default.
• W2052690206 cites W2168297954 @default.
• W2052690206 cites W2168751120 @default.
• W2052690206 cites W2172305519 @default.
• W2052690206 cites W2176978061 @default.
• W2052690206 cites W3198712657 @default.
• W2052690206 doi "https://doi.org/10.1016/j.epsl.2010.08.002" @default.
• W2052690206 hasPublicationYear "2010" @default.
• W2052690206 type Work @default.
• W2052690206 sameAs 2052690206 @default.
• W2052690206 citedByCount "20" @default.
• W2052690206 countsByYear W20526902062012 @default.
• W2052690206 countsByYear W20526902062013 @default.
• W2052690206 countsByYear W20526902062015 @default.
• W2052690206 countsByYear W20526902062017 @default.
• W2052690206 countsByYear W20526902062018 @default.
• W2052690206 countsByYear W20526902062019 @default.
• W2052690206 countsByYear W20526902062020 @default.
• W2052690206 countsByYear W20526902062021 @default.
• W2052690206 countsByYear W20526902062022 @default.
• W2052690206 countsByYear W20526902062023 @default.

• next