Database dump for this sample:
Top depth (cm) 50.0
Bottom depth (cm) 54.0
Lithology Mud with highly rhythmic, but faint submm- to mm-scale laminae and common gravel-sized clasts. Moderate opal (around 10 percent), TOC content (around 0.25 percent), and high water content (around 45 percent). Clasts include: quartz, feldspars, granite,basalt, dolerite,metamorphic lithologies (foliated/mylontic granitoids, metasediments, marble). Benthic and planktonic forams present. Common diatoms (0.74 * 10^9 valves/g).
Facies interpretation Common diatom content and gravel clasts alongside the planktonic/benthic foraminifera suggests a short duration period of pelagic sedimentation in open water with iceberg rafting over the core site. Rhythmic laminae suggest traction currents reworking hemipelagic suspension settling sediments or turbidites (see facies Ml). We interpret that the input of terrigenous material has allowed this short-lived interval to be preserved in the stratigraphy, where as higher in the stratigraphic succession (e.g. Facies Mb), sediment starvation (due to a lack of terrigenous sediment supply) combined with bioturbation does not allow for the preservation of such events.
Core sample comments None
Carbon type benthic foraminifera
Analysis date None
Chem lab None
Analyst None
Sample preparation method None
AMS lab Rafter Radiocarbon Lab
AMS date None
Analysis ID NZA50804
Percent carbon None
Fraction modern None
δ13C (‰) None
14C age (yr) 8892.0
14C age uncertainty (yr) 155.0
14C comments None

Calibration results:
Calibration curveMarine20
Reservoir correction (14C yr BP) (mean and st.dev. of all Antarctica calibration samples) (http://calib.org/marine/)1141 ± 179
Calibration softwareIOSACal (v.0.5.3)
Calibrated age 95.45 % HPD interval(s) (yr)8561.0 to 7549.0 cal yr BP
Calibrated age 68.2 % HPD interval(s) (yr)8296.0 to 7792.0 cal yr BP
14C calibration plot



Questions about this page: Ryan Venturelli