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        <gco:CharacterString>STUDY NOTES: Boron/Calcium data for benthic foraminifera from the Eocene-Oligocene of Ocean Drilling Program Sites 689, 690 (Maud Rise), and Site 1262 (Walvis Ridge). Analyses were carried out by ICPMS. ODP Site 689: 64°31.020'S, 3°5.994' E, 2080m water depth ODP Site 690: 65° 9.629'S, 1°12.296'E, 2914m water depth ODP Site 1262: 27°11.160'S, 1°34.620'E, 4755m water depth 
ABSTRACT SUPPLIED BY ORIGINATOR: We present modern B/Ca core-top calibrations for the epifaunal benthic foraminifer Nuttallides umbonifera and the infaunal Oridorsalis umbonatus to test whether B/Ca values in these species can be used for the reconstruction of paleo-Δ[CO32−]. O. umbonatus originated in the Late Cretaceous and remains extant, whereas N. umbonifera originated in the Eocene and is the closest extant relative to Nuttallides truempyi, which ranges from the Late Cretaceous through the Eocene. We measured B/Ca in both species in 35 Holocene sediment samples from the Atlantic, Pacific and Southern Oceans. B/Ca values in epifaunal N. umbonifera (~ 85–175 μmol/mol) are consistently lower than values reported for epifaunal Cibicidoides (Cibicides) wuellerstorfi (130–250 μmol/mol), though the sensitivity of Δ[CO32−] on B/Ca in N. umbonifera (1.23 ± 0.15) is similar to that in C. wuellerstorfi (1.14 ± 0.048). In addition, we show that B/Ca values of paired N. umbonifera and its extinct ancestor, N. truempyi, from Eocene cores are indistinguishable within error. In contrast, both the B/Ca (35–85 μmol/mol) and sensitivity to Δ[CO32−] (0.29 ± 0.20) of core-top O. umbonatus are considerably lower (as in other infaunal species), and this offset extends into the Paleocene. Thus the B/Ca of N. umbonifera and its ancestor can be used to reconstruct bottom water Δ[CO32−], whereas O. umbonatus B/Ca appears to be buffered by porewater [CO32−] and suited for constraining long-term drift in seawater B/Ca.</gco:CharacterString>
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