TY - JOUR
T1 - A dataset of the mid-brunhes period at site MD05-2925, Solomon Sea
T2 - Surface-subsurface planktonic foraminifera stable C-O isotope and Mg/Ca ratios
AU - Lo, Li
AU - Chang, Tzu Ling
AU - Su, Yu Chu
AU - Chuang, Chih Kai
AU - Shen, Chuan Chou
AU - Mii, Horng Sheng
N1 - Publisher Copyright:
© 2021
PY - 2021/10
Y1 - 2021/10
N2 - 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 µm) and Pulleniatina obliquiloculata (355–425 µm) tests were hand-picked and cleaned for stable carbon and oxygen isotopes and Mg/Ca analyses. Composite benthic foraminifera tests (>250 µm, 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.
AB - 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 µm) and Pulleniatina obliquiloculata (355–425 µm) tests were hand-picked and cleaned for stable carbon and oxygen isotopes and Mg/Ca analyses. Composite benthic foraminifera tests (>250 µm, 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.
KW - Benthic foraminifera
KW - Carbon isotope
KW - Marine Isotope Stage 11
KW - Mg/Ca ratios
KW - Oxygen isotope stratigraphy
KW - Planktonic foraminifera
KW - Seawater oxygen isotope
KW - Solomon Sea
UR - http://www.scopus.com/inward/record.url?scp=85112406016&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85112406016&partnerID=8YFLogxK
U2 - 10.1016/j.dib.2021.107283
DO - 10.1016/j.dib.2021.107283
M3 - Article
AN - SCOPUS:85112406016
SN - 2352-3409
VL - 38
JO - Data in Brief
JF - Data in Brief
M1 - 107283
ER -