This core appears in the following publications:

Bart, Philip J and DeCesare, Matthew and Rosenheim, Brad E and Majewski, Wojceich and McGlannan, Austin
A centuries-long delay between a paleo-ice-shelf collapse and grounding-line retreat in the Whales Deep Basin, eastern Ross Sea, Antarctica
Scientific reports, 2018
DOI: 10.1038/s41598-018-29911-8
Cores in
this publication

Core-related info:
Core name 012-KC
Setting marine
RegionWhales Deep Basin, Ross Sea
Collection date 2015-03-20
IGSN ID ARF000HMC
Core type kasten
Latitude -76.16097
Longitude -169.00108
Water depth (m) 596.0
Core length (cm) 252.0
Comments None

Cruise-related info:
CruiseNBP15-02B
Ship Nathaniel B. Palmer
Cruise start date 2015-01-23
Cruise end date 2015-03-16

Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
3300 38.0 - 42.0 sub-ice shelf mixed benthic foraminifera 12950.0 ± 65.0
3301 53.0 - 58.0 sub-ice shelf Foraminifera (T. earlandi) 13405.0 ± 120.0
3302 97.0 - 102.0 sub-ice shelf mixed benthic foraminifera 13200.0 ± 75.0
3303 215.0 - 220.0 diamict Either subglacial or grounding-line proximal setting. Foraminifera (G. biora) 44837.0 ± 4200.0

Depth-age relationship:
Plot key: black and gray bars represent 68.2% and 95.45% HPD interval(s), respectively.

Questions about this page: Ryan Venturelli