FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2525881489> ?p ?o ?g. }

• W2525881489 endingPage "150" @default.
• W2525881489 startingPage "141" @default.
• W2525881489 abstract "The last 150 years on the California margin have been marked by high variability in precipitation, temperature, sea surface temperature, and ocean chemistry, in response to both natural and anthropogenic changes. Deciphering climate history from ocean sediments is dependent on our understanding of the various influences on marine proxies. Sediment from Santa Barbara Basin (SBB), California (box core SPR0901-10BC) provides an opportunity to compare multiple marine proxies with instrumental records of climate of the past 150 years and extend them beyond the historical record. Here we use three planktonic foraminiferal proxies, δ18Ocalcite, Mg/Ca, and size-normalized shell weight, to reconstruct the surface temperature and δ18Owater in SBB California at near-annual resolution from AD 1850–2000. Results indicate that Globigerina bulloides Mg/Ca reflects the instrumental temperature trends over the last 150 years, with average Mg/Ca temperatures approximately 2 °C lower than instrumental values, due to the slightly deeper habitat preference of G. bulloides. Similarly, temperature is the dominant control on G. bulloides δ18Ocalcite, and both Mg/Ca and δ18Ocalcite reflect variability consistent with changes in the intensification of ENSO over the past 150 years. Shell weights of the planktic foraminifer G. bulloides are inversely correlated with historical sea surface temperatures over the last 150 years in SBB sediments. Greater shell weight associated with cooler surface ocean temperatures does not support the anticipated relationship between coastal upwelling of cool, low pH water and shell thinning due to CO32− undersaturation. However, in contrast to the previous 130 years, G. bulloides shells deposited on the sea floor since the late 1970s exhibit a distinctive smooth shell structure indicative of partial dissolution. We hypothesize that a mid-1970s shift in intermediate water flow from predominantly equatorward to anomalously poleward led to the influx of relatively corrosive bottom water into SBB with subsequent carbonate dissolution at the sediment–water interface." @default.
• W2525881489 created "2016-10-07" @default.
• W2525881489 creator A5019136974 @default.
• W2525881489 creator A5040793891 @default.
• W2525881489 creator A5053257911 @default.
• W2525881489 creator A5061100164 @default.
• W2525881489 creator A5078552776 @default.
• W2525881489 date "2018-03-01" @default.
• W2525881489 modified "2023-10-13" @default.
• W2525881489 title "Foraminiferal proxy response to ocean temperature variability and acidification over the last 150 years in the Santa Barbara Basin (California)" @default.
• W2525881489 cites W1489155911 @default.
• W2525881489 cites W1510718267 @default.
• W2525881489 cites W1552172549 @default.
• W2525881489 cites W1556275511 @default.
• W2525881489 cites W1602484435 @default.
• W2525881489 cites W1636092099 @default.
• W2525881489 cites W1743880976 @default.
• W2525881489 cites W1919029059 @default.
• W2525881489 cites W1955284625 @default.
• W2525881489 cites W1968988439 @default.
• W2525881489 cites W1976061944 @default.
• W2525881489 cites W1983988867 @default.
• W2525881489 cites W1991287814 @default.
• W2525881489 cites W1994066060 @default.
• W2525881489 cites W1997626537 @default.
• W2525881489 cites W2003473594 @default.
• W2525881489 cites W2005341723 @default.
• W2525881489 cites W2006041837 @default.
• W2525881489 cites W2006149841 @default.
• W2525881489 cites W2008419017 @default.
• W2525881489 cites W2013513194 @default.
• W2525881489 cites W2016736393 @default.
• W2525881489 cites W2020883805 @default.
• W2525881489 cites W2022530745 @default.
• W2525881489 cites W2022633352 @default.
• W2525881489 cites W2026128738 @default.
• W2525881489 cites W2028776183 @default.
• W2525881489 cites W2043460413 @default.
• W2525881489 cites W2050103984 @default.
• W2525881489 cites W2050947086 @default.
• W2525881489 cites W2055987266 @default.
• W2525881489 cites W2059111217 @default.
• W2525881489 cites W2060012482 @default.
• W2525881489 cites W2062296330 @default.
• W2525881489 cites W2068375361 @default.
• W2525881489 cites W2079538883 @default.
• W2525881489 cites W2079868285 @default.
• W2525881489 cites W2081226145 @default.
• W2525881489 cites W2081756558 @default.
• W2525881489 cites W2089127299 @default.
• W2525881489 cites W2093401535 @default.
• W2525881489 cites W2094350389 @default.
• W2525881489 cites W2098759916 @default.
• W2525881489 cites W2108527489 @default.
• W2525881489 cites W2113297575 @default.
• W2525881489 cites W2117744771 @default.
• W2525881489 cites W2122451984 @default.
• W2525881489 cites W2139382400 @default.
• W2525881489 cites W2141948084 @default.
• W2525881489 cites W2164642034 @default.
• W2525881489 cites W2168062665 @default.
• W2525881489 doi "https://doi.org/10.1016/j.quaint.2016.07.049" @default.
• W2525881489 hasPublicationYear "2018" @default.
• W2525881489 type Work @default.
• W2525881489 sameAs 2525881489 @default.
• W2525881489 citedByCount "6" @default.
• W2525881489 countsByYear W25258814892017 @default.
• W2525881489 countsByYear W25258814892020 @default.
• W2525881489 countsByYear W25258814892021 @default.
• W2525881489 countsByYear W25258814892022 @default.
• W2525881489 countsByYear W25258814892023 @default.
• W2525881489 crossrefType "journal-article" @default.
• W2525881489 hasAuthorship W2525881489A5019136974 @default.
• W2525881489 hasAuthorship W2525881489A5040793891 @default.
• W2525881489 hasAuthorship W2525881489A5053257911 @default.
• W2525881489 hasAuthorship W2525881489A5061100164 @default.
• W2525881489 hasAuthorship W2525881489A5078552776 @default.
• W2525881489 hasBestOaLocation W25258814891 @default.
• W2525881489 hasConcept C109007969 @default.
• W2525881489 hasConcept C111368507 @default.
• W2525881489 hasConcept C11864286 @default.
• W2525881489 hasConcept C119857082 @default.
• W2525881489 hasConcept C122846477 @default.
• W2525881489 hasConcept C127313418 @default.
• W2525881489 hasConcept C134097258 @default.
• W2525881489 hasConcept C149348798 @default.
• W2525881489 hasConcept C151730666 @default.
• W2525881489 hasConcept C2775838028 @default.
• W2525881489 hasConcept C2780148112 @default.
• W2525881489 hasConcept C2780368712 @default.
• W2525881489 hasConcept C41008148 @default.
• W2525881489 hasConcept C49204034 @default.
• W2525881489 hasConcept C83042747 @default.
• W2525881489 hasConceptScore W2525881489C109007969 @default.
• W2525881489 hasConceptScore W2525881489C111368507 @default.
• W2525881489 hasConceptScore W2525881489C11864286 @default.
• W2525881489 hasConceptScore W2525881489C119857082 @default.
• W2525881489 hasConceptScore W2525881489C122846477 @default.

• next