Database dump for this sample:
Top depth (cm) 101.0
Bottom depth (cm) 102.0
Lithology Muddy Diamict, low opal (5 percent), TOC content (<0.25 percent), and low water content (around 15-20 percent). Clasts include: quartz, dolerite, granite,metamorphic lithologies (foliated/mylontic granitoids, metasediments, biotite schists, marble). Highly fragmented diatoms (0.3 * 10^9 valves/g).
Facies interpretation Subglacial transport and deposition in a subglacial or a grounding line proximal depositional setting (i.e. subglacial basal debris melt out). Lowest values of diatom and opal (but still high relative to other tills in antarctica, suggesting reworking of older diatom oozes), TOC and water content similar to other diamicts interpreted as tills elsewhere in the Ross Sea (Licht et al., 1996; Anderson, 1999; Domack et al., 1999, Mckay et al., 2008) and the Antarctic margin ((Smith et al., 2011)).
Core sample comments None
Carbon type AIO
Analysis date None
Chem lab None
Analyst None
Sample preparation method None
AMS lab Rafter Radiocarbon Lab
AMS date None
Analysis ID NZA37581
Percent carbon None
Fraction modern None
δ13C (‰) None
14C age (yr) 33050.0
14C age uncertainty (yr) 390.0
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.0.6.0)
Calibrated age 95.45 % HPD interval(s) (yr)36362.0 to 34584.0 cal yr BP
Calibrated age 68.2 % HPD interval(s) (yr)36013.0 to 35121.0 cal yr BP
14C calibration plot



Questions about this page: Ryan Venturelli