FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2613290103> ?p ?o ?g. }

• W2613290103 endingPage "530" @default.
• W2613290103 startingPage "512" @default.
• W2613290103 abstract "The carbon isotope composition (δ13C) of seawater provides valuable insight on ocean circulation, air-sea exchange, the biological pump, and the global carbon cycle and is reflected by the δ13C of foraminifera tests. Here more than 1700 δ13C observations of the benthic foraminifera genus Cibicides from late Holocene sediments (δ13CCibnat) are compiled and compared with newly updated estimates of the natural (preindustrial) water column δ13C of dissolved inorganic carbon (δ13CDICnat) as part of the international Ocean Circulation and Carbon Cycling (OC3) project. Using selection criteria based on the spatial distance between samples, we find high correlation between δ13CCibnat and δ13CDICnat, confirming earlier work. Regression analyses indicate significant carbonate ion (−2.6 ± 0.4) × 10−3‰/(μmol kg−1) [CO32−] and pressure (−4.9 ± 1.7) × 10−5‰ m−1 (depth) effects, which we use to propose a new global calibration for predicting δ13CDICnat from δ13CCibnat. This calibration is shown to remove some systematic regional biases and decrease errors compared with the one-to-one relationship (δ13CDICnat = δ13CCibnat). However, these effects and the error reductions are relatively small, which suggests that most conclusions from previous studies using a one-to-one relationship remain robust. The remaining standard error of the regression is generally σ ≅ 0.25‰, with larger values found in the southeast Atlantic and Antarctic (σ ≅ 0.4‰) and for species other than Cibicides wuellerstorfi. Discussion of species effects and possible sources of the remaining errors may aid future attempts to improve the use of the benthic δ13C record." @default.
• W2613290103 created "2017-05-19" @default.
• W2613290103 creator A5000019906 @default.
• W2613290103 creator A5001481194 @default.
• W2613290103 creator A5003176718 @default.
• W2613290103 creator A5003682711 @default.
• W2613290103 creator A5005219457 @default.
• W2613290103 creator A5013272069 @default.
• W2613290103 creator A5019280918 @default.
• W2613290103 creator A5030337929 @default.
• W2613290103 creator A5033425589 @default.
• W2613290103 creator A5035018620 @default.
• W2613290103 creator A5036484370 @default.
• W2613290103 creator A5042721126 @default.
• W2613290103 creator A5045138236 @default.
• W2613290103 creator A5063819125 @default.
• W2613290103 creator A5071535930 @default.
• W2613290103 creator A5073629607 @default.
• W2613290103 creator A5078709597 @default.
• W2613290103 creator A5081293312 @default.
• W2613290103 creator A5085348552 @default.
• W2613290103 creator A5087287878 @default.
• W2613290103 creator A5087615628 @default.
• W2613290103 creator A5087925100 @default.
• W2613290103 creator A5091455900 @default.
• W2613290103 date "2017-06-01" @default.
• W2613290103 modified "2023-10-16" @default.
• W2613290103 title "Calibration of the carbon isotope composition (δ ¹³ C) of benthic foraminifera" @default.
• W2613290103 cites W1487001512 @default.
• W2613290103 cites W1489155911 @default.
• W2613290103 cites W1511313527 @default.
• W2613290103 cites W1580457452 @default.
• W2613290103 cites W1585334448 @default.
• W2613290103 cites W1598455849 @default.
• W2613290103 cites W1609491364 @default.
• W2613290103 cites W1611443029 @default.
• W2613290103 cites W1658156290 @default.
• W2613290103 cites W1861860560 @default.
• W2613290103 cites W1895999970 @default.
• W2613290103 cites W1982701446 @default.
• W2613290103 cites W1984667039 @default.
• W2613290103 cites W1989866434 @default.
• W2613290103 cites W2005878063 @default.
• W2613290103 cites W2009429119 @default.
• W2613290103 cites W2016225258 @default.
• W2613290103 cites W2018069199 @default.
• W2613290103 cites W2024597018 @default.
• W2613290103 cites W2025514072 @default.
• W2613290103 cites W2025790067 @default.
• W2613290103 cites W2029783693 @default.
• W2613290103 cites W2036351156 @default.
• W2613290103 cites W2036793100 @default.
• W2613290103 cites W2039648311 @default.
• W2613290103 cites W2041604895 @default.
• W2613290103 cites W2043358023 @default.
• W2613290103 cites W2045768221 @default.
• W2613290103 cites W2046359238 @default.
• W2613290103 cites W2052727776 @default.
• W2613290103 cites W2058313183 @default.
• W2613290103 cites W2058931034 @default.
• W2613290103 cites W2062302144 @default.
• W2613290103 cites W2066870541 @default.
• W2613290103 cites W2070594612 @default.
• W2613290103 cites W2075520347 @default.
• W2613290103 cites W2080392490 @default.
• W2613290103 cites W2081056855 @default.
• W2613290103 cites W2083740890 @default.
• W2613290103 cites W2084349604 @default.
• W2613290103 cites W2090767277 @default.
• W2613290103 cites W2091524823 @default.
• W2613290103 cites W2093142430 @default.
• W2613290103 cites W2093722277 @default.
• W2613290103 cites W2095493295 @default.
• W2613290103 cites W2095861329 @default.
• W2613290103 cites W2103170649 @default.
• W2613290103 cites W2118977549 @default.
• W2613290103 cites W2121956394 @default.
• W2613290103 cites W2122249284 @default.
• W2613290103 cites W2133697952 @default.
• W2613290103 cites W2152188824 @default.
• W2613290103 cites W2156865657 @default.
• W2613290103 cites W2186068922 @default.
• W2613290103 cites W2499871837 @default.
• W2613290103 cites W2550999150 @default.
• W2613290103 cites W311622389 @default.
• W2613290103 cites W330812554 @default.
• W2613290103 cites W4248989118 @default.
• W2613290103 cites W55697062 @default.
• W2613290103 cites W641797458 @default.
• W2613290103 cites W77819027 @default.
• W2613290103 doi "https://doi.org/10.1002/2016pa003072" @default.
• W2613290103 hasPublicationYear "2017" @default.
• W2613290103 type Work @default.
• W2613290103 sameAs 2613290103 @default.
• W2613290103 citedByCount "52" @default.
• W2613290103 countsByYear W26132901032017 @default.
• W2613290103 countsByYear W26132901032018 @default.
• W2613290103 countsByYear W26132901032019 @default.

• next