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  4. A dataset of the mid-brunhes period at site MD05-2925, Solomon Sea: Surface-subsurface planktonic foraminifera stable C-O isotope and Mg/Ca ratios
 
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A dataset of the mid-brunhes period at site MD05-2925, Solomon Sea: Surface-subsurface planktonic foraminifera stable C-O isotope and Mg/Ca ratios

Journal
Data in Brief
Journal Volume
38
Date Issued
2021
Author(s)
Lo L.  
Chang T.-L
Su Y.-C
Chuang C.-K
CHUAN-CHOU SHEN  
Horng-Sheng Mii
DOI
10.1016/j.dib.2021.107283
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85112406016&doi=10.1016%2fj.dib.2021.107283&partnerID=40&md5=5194f667bdc5dfc9d2df39fee4de3efc
https://scholars.lib.ntu.edu.tw/handle/123456789/606211
Abstract
Here we present derived thermal-hydrological variations data during the Marine isotope stages (MISs) 10–12 using surface and subsurface dwelling planktonic foraminiferal geochemical proxies of a sedimentary core of MD05-2925 (9.3oS, 151.5oE, water depth 1661 m, core depth 1842–2430 cm), Solomon Sea. Globigerinoides ruber (s.s., white, 250–300 ?m) and Pulleniatina obliquiloculata (355–425 ?m) tests were hand-picked and cleaned for stable carbon and oxygen isotopes and Mg/Ca analyses. Composite benthic foraminifera tests (>250 ?m, Uvigerina spp., and Bulimina spp.) are also hand-picked and cleaned for stable oxygen isotope stratigraphy. In total, 235 and 148 measurements for C-O stable isotopes and Mg/Ca ratios for planktonic foraminifera in 2–5 cm resolution for the period from 352.1 to 462.3 ka are presented in this data report, respectively. Age model is established by tuning composite benthic foraminiferal oxygen isotope to global composite benthic foraminifera oxygen isotope stack LR04. Surface and subsurface temperatures and seawater oxygen isotopes (δ18OW, without ice volume correction) were calculated. ? 2021
Subjects
Benthic foraminifera
Carbon isotope
Marine Isotope Stage 11
Mg/Ca ratios
Oxygen isotope stratigraphy
Planktonic foraminifera
Seawater oxygen isotope
Solomon Sea
SDGs

[SDGs]SDG13

[SDGs]SDG14

Type
data paper

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