Appendix A Table SD1. CaCO3, δ¹⁸O, δ¹³C and Sr isotopes from ODP Site 181-1120

An integrated chemostratigraphic (87Sr/86Sr, d13C and 18O) study of benthic foraminifera is presented for a 210 m-thick, intermediate depth (upper/middle bathyal transition), Miocene nannofossil ooze section of Ocean Drilling Program Site 1120, Campbell Plateau off New Zealand. Our results indicate...

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Bibliographic Details
Main Authors: Ando, Atsushi, Khim, Boo-Keun, Nakano, Takanori, Takata, Hiroyuki
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
181-1120B
181-1120D
Calcium carbonate
Cibicidoides spp.
δ13C
δ18O
Comment
DEPTH
sediment/rock
DRILL
Drilling/drill rig
Event label
Finnigan TRITON thermal ionization mass spectrometer (TIMS)
Joides Resolution
Leg181
Mass spectrometer Finnigan MAT 251
Ocean Drilling Program
ODP
Period (Geological Time Scale)
Sample code/label
South Pacific Ocean
Strontium-87/Strontium-86 ratio
error
Campbell Plateau
New Zealand
Pacific
Southern Ocean
Triton
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.763934
https://doi.org/10.1594/PANGAEA.763934
Description
Summary:An integrated chemostratigraphic (87Sr/86Sr, d13C and 18O) study of benthic foraminifera is presented for a 210 m-thick, intermediate depth (upper/middle bathyal transition), Miocene nannofossil ooze section of Ocean Drilling Program Site 1120, Campbell Plateau off New Zealand. Our results indicate that new 87Sr/86Sr, d13C and d18O profiles are wholly consistent with their respective Miocene reference curves. These observations facilitate identification of a total of five reliable chemostratigraphic datums, which are based on the fundamental structural changes in the 87Sr/86Sr curve and paired simultaneous d13C and d18O events. The resultant age-depth relationship clearly shows that the Miocene (20-5 Ma) biopelagic sedimentation on the Campbell Plateau was essentially continuous at a moderate to high, linear sedimentation rate (17.5 m/m.y. with an exception of the uppermost 13 m). Our findings do not support the shipboard biostratigraphic age model, which assumes that the critical early-middle Miocene transition was interrupted by a major hiatus (<~3 m.y.). Because of its unique bathymetric setting at a paleowater-depth of ~ 600 m, which is among the shallowest of the coeval isotopically studied deep-sea sections in the South Pacific/Southern Ocean, Site 1120 will serve as a reference section for surveying the evolution of intermediate-water paleoceanography in the Southern Hemisphere across the middle Miocene climatic transition.

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