(Table T2) Stable iron isotope ratios and amount of iron extracted by different methods from ODP Site 207-1260 sediments

Fe isotope measurements are presented for 10 samples from the Cenomanian-Turonian black shale unit in Hole 1260B at Demerara Rise. The samples bracket the latest Cenomanian ocean anoxic event and were selected to ascertain whether Fe isotopes can be used to gain a better understanding of oceanic red...

Full description

Bibliographic Details
Main Authors: Clayton, Robin E, Nederbragt, Alexandra J, Malinovsky, Dmitry, Andersson, Per S, Thurow, Juergen W
Format: Dataset
Language:English
Published: PANGAEA 2006
Subjects:
207-1260
COMPCORE
Composite Core
DEPTH
sediment/rock
DSDP/ODP/IODP sample designation
Iron
Joides Resolution
Leg207
MC-ICP-MS Thermo-Finnigan Neptune
North Atlantic Ocean
Ocean Drilling Program
ODP
Percentage
Sample code/label
Weighted
δ56Fe
standard deviation
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.776004
https://doi.org/10.1594/PANGAEA.776004
Description
Summary:Fe isotope measurements are presented for 10 samples from the Cenomanian-Turonian black shale unit in Hole 1260B at Demerara Rise. The samples bracket the latest Cenomanian ocean anoxic event and were selected to ascertain whether Fe isotopes can be used to gain a better understanding of oceanic redox conditions during the mid-Cretaceous. Three extraction procedures were used to provide Fe extracts that represent the Fe oxide (average FeCBD = 0.07 wt%, N = 8), Fe oxide-sulfide-carbonate (average FeAR = 0.34 wt%, N = 10), and total Fe fractions (average FeHF = 0.81 wt%, N = 10). Fe isotope measurements were conducted on all FeAR extracts as a priority as these were considered to best reflect changes in the redox environment. d56Fe values range between 0.02 per mil ± 0.09 per mil and -0.77 per mil ± 0.05 per mil and appear to correlate negatively with the C/N ratio and oxygen index of total organic carbon. Isotopic measurements of two Fe oxide (FeCBD) extracts show a much heavier isotopic composition (d56Fe = 0.74 per mil ± 0.08 per mil and 0.63 per mil ± 0.04 per mil), which suggests isotopic partitioning between different mineral components in the sediment.

Similar Items