Associated publications

Title Author(s) Publication DOI View cores
Late Cenozoic glacial-marine, carbonate, and turbidite sedimentation in the northwestern Ross Sea, Antarctica Reid, David Eugene , 1989 https://www.proquest.com/docview/194016843/fulltextPDF/306796DA039B49D7PQ/1?accountid=25386&sourcetype=Dissertations%20&%20Theses

Core information

Core name Region Collection date IGSN ID Core type Latitude (DD) Longitude (DD) Water depth
(m)
Core length
(m)
Comments
DF87-14 Antarctica, Ross Sea None Piston -72.97283 -179.89250 658.0 1.79 Coarse ash abundant throughout; sand and ash content inccreases with depth; layer of ash bearing foraminiferal ooze, light olive gray (5Y 5/2), between 31-35 cm; slightly bioturbated between 39-44 cm and 70-78cm; highly disturbed between 0-13 cm; moderately disturbed between 19-21 cm; gradational contact. ; Coarse ash abundant; fine to medium subangular to subrounded pebbles of various compositions sparsely scattered throughout; very fine angular to subroinded pebbles of various compositions common throughout; ;ayer of foraminiferal sany, olive gray (5Y 4/1) between 104-115 cm, sand is fine, well sorted, upper and lower contacts are sharp and inclined; inclined laminae of foraminiferal ooze, yellowish gray (5Y 7/2), between 103-104 cm; slightly disturbed between 131-133 cm; sharp contact.; Moderate olive brown (5Y 4/4); sand is fine, well sorted; coarse ash abundant throughout; very fine subangular to subrounded pebbles of various compositions common throughout; 8 cm sedimentary clast composed of mud and sandy mud, grayish olive (10Y 4/2); moderately bioturbated between 147-158 cm.; Reported as >35,410 14C yrs BP

Expedition information

Expedition name Ship Start date End date Report DOI
DF87 USCGC Glacier Dec. 17, 1986 Jan. 16, 1987 https://osu-mgr.org/OSU-DF87

Samples in this core

Sample ID Core depth
(m)
Lithology Facies interpretation Carbon type Sample preparation type Age (14C yr ± 1σ) Calibrated age, median probability (cal. yr BP) Calibrated age, 2σ range (cal. yr BP) Comments
DF87-14_5-9 0.05 - 0.09 Foraminiferal ooze Carbonate sedimentation during LGM, low clastic sedimentation, high nutrient supply, seasonal open marine during LGM, east to west increase in current strength, winnowed and current swept seafloor Foraminifera (mostly N. pachyderma, some benthics), barnacle fragments Carbonate hydrolysis 35410.0 ± None Calibrated age for default reservoir correction not available Calibrated age for default reservoir correction not available None

Associated documents

No associated documents.