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Teitler, Lora; Warnke, Detlef A; Venz, Kathryn A; Hodell, David A; Becquey, Sabine; Gersonde, Rainer; Teitler, Winston (2022): Iceberg-Rafted Debris data from South Atlantic for study of Antarctic Ice Sheet stability over last ~500 kyrs [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.948709

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Abstract:
This database contains the data resulting from a study of Antarctic Ice Sheet history, over the last ~500 thousand years. Iceberg-rafted debris (IRD), considered as an indicator of the presence of a continental ice sheet in the source area, is counted and analyzed in relation to the other components of the studied size fraction. The study materials are derived from two cores raised from a deep-water marine site in the southeastern Atlantic Ocean: the piston core TN057-6-PC4 and the associated drill core from the Ocean Drilling Program (ODP) Leg 177 Site 1090 (177-1090). Because the top portion of the 177-1090 drill core was apparently disturbed by the drilling, the piston core TN057-6-PC4 has been used to represent the most recent part of the record. The site is located at ~43 deg S, 9 deg E, about 2/3 of the way from the Antarctic coast to South Africa. The location from which both cores were raised is on the southern slope of the Agulhas Ridge, on the northern edge of the Agulhas Basin, in the southeastern Atlantic Ocean.
The initial cleaning and preparation of samples from these cores was carried out by Kathryn Venz and David Hodell (UF). The methods used here to examine the IRD are those described by Allen and Warnke (1991, doi:10.2973/odp.proc.sr.114.118.1991), Stanton (1997), and Murphy et al. (2002, doi:10.1016/S0031-0182(01)00495-3). The samples were first weighed, then separated by sieving into four size fractions: <150 microns, 150-250 microns, 250 microns to 2 mm, and >2 mm. The medium to coarse sand size fraction (250 microns to 2 mm) was utilized for our study. Within this, a split of about 1000 grains was obtained; the grains in this split were counted. Grains that were counted within categories that included: quartz, feldspar, mafic minerals, lithic fragments, volcanic lithics, volcanic ash, diatoms, planktic forams, benthic forams, radiolarians, and 'other'. The counts of quartz, feldspar, mafic minerals and lithic non-volcanic fragments were then summed as IRD. Following the suggestion of Murphy et al. (2002), the final step of this stage was a brief overview of the non-counted portion of the 250 micron to 2 mm size fraction, primarily to look for 'background rafting'. Background rafting refers to the presence of IRD in the non-counted portion (i.e., outside of the counted split) of the size fraction. For this study, a note was made of the presence or absence only of any IRD clasts in the non-counted portion.
Keyword(s):
Antarctic ice sheet stability; iceberg rafted debris; ODP 177-1090; ODP TN0576-PC4
Related to:
Teitler, Lora; Warnke, Detlef A; Venz, Kathryn A; Hodell, David A; Becquey, Sabine; Gersonde, Rainer; Teitler, Winston (2010): Determination of Antarctic Ice Sheet stability over the last ∼500 ka through a study of iceberg-rafted debris. Paleoceanography, 25(1), https://doi.org/10.1029/2008PA001691
Further details:
Stanton, Cathy (1997): History of ice rafted debris at ODP Leg 162, Site 982, in the North Atlantic for the past 2 million years [thesis]. California State University, Hayward, Hayward, CA
Project(s):
Coverage:
Median Latitude: -42.913533 * Median Longitude: 8.799900 * South-bound Latitude: -42.913700 * West-bound Longitude: 8.600000 * North-bound Latitude: -42.913300 * East-bound Longitude: 8.900000
Date/Time Start: 1997-12-26T15:22:00 * Date/Time End: 1997-12-30T00:55:00
Minimum DEPTH, sediment/rock: 0.030 m * Maximum DEPTH, sediment/rock: 17.010 m
Event(s):
177-1090B * Latitude: -42.913700 * Longitude: 8.899700 * Date/Time Start: 1997-12-26T15:22:00 * Date/Time End: 1997-12-28T14:55:00 * Elevation: -3699.4 m * Penetration: 397.5 m * Recovery: 373.23 m * Location: South Atlantic Ocean * Campaign: Leg177 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 43 cores; 397.5 m cored; 0 m drilled; 93.9 % recovery
177-1090D * Latitude: -42.913600 * Longitude: 8.900000 * Date/Time Start: 1997-12-28T23:25:00 * Date/Time End: 1997-12-30T00:55:00 * Elevation: -3702.1 m * Penetration: 225.9 m * Recovery: 213.64 m * Location: South Atlantic Ocean * Campaign: Leg177 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 225.9 m cored; 0 m drilled; 94.6 % recovery
TN057-6-PC4 * Latitude: -42.913300 * Longitude: 8.600000 * Elevation Start: -3751.0 m * Elevation End: -3701.6 m * Recovery: 12.76 m * Method/Device: Piston corer (PC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventTeitler, Lora
2Sample code/labelSample labelTeitler, LoraDSDP/ODP/IODP sample designation
3SectionSectTeitler, Lora
4Depth, sectionDepth sectcmTeitler, Lora
5DEPTH, sediment/rockDepth sedmTeitler, LoraIODP Depth Scale TerminologyGeocode – mbsf
6Size fraction 2-0.250 mm, coarser sand2000-250 µmgTeitler, Lora
7Number of subsamplesSubsamples#Teitler, Lora# of splits of size fraction to obtain a split of ~1000 grains
8QuartzQz#Teitler, LoraCounted
9FeldsparFsp#Teitler, LoraCounted
10Mafic mineralsMafic min#Teitler, LoraCounted
11Lithic grainsLithic#Teitler, LoraCountedNon-volcanic lithics other than Qz, Fsp, or Mafic
12Lithic grains, volcanicLithic volc#Teitler, LoraCounted
13Tephra or volcanic ashTephra#Teitler, LoraCounted
14DiatomsDiatoms#Teitler, LoraCounted
15Foraminifera, plankticForam plankt#Teitler, LoraCounted
16Foraminifera, benthicForam benth#Teitler, LoraCounted
17RadiolariansRad#Teitler, LoraCounted
18Grains, othergrains other#Teitler, LoraCounted
19Grains, counted/analyzedGrains#Teitler, LoraCalculatedTotal grains count (in split)
20Garnets, presence/absenceGarnets presenceTeitler, LoraPresence of garnets (yes=1, no=0)
21Dictyocoryne profunda, presence/absenceD. profunda presenceTeitler, LoraPresence of D. profunda (yes=0.8, no=0)
22Sample commentSample commentTeitler, Lora
23Iceberg rafted debris grains, total, in subsampleTIRD grains subsample#Teitler, LoraCalculatedTIRD{split} = Qz + Fsp + Mafic + Lithic counts
24Iceberg rafted debris indexIRD indexTeitler, LoraCalculateddefined as a percent: IRDI = [TIRD{split} / (TIRD{split} + Foram plankt{split})] × 100
25AGEAgeka BPTeitler, LoraAdopted from Hodell et al. (2000); Venz and Hodell (2002)Geocode
26Sedimentation rateSRcm/kaTeitler, LoraCalculatedSedRate = depth increment (sample, in cm)/age increment (sample, kyr)
27Iceberg rafted debris grains/total grains ratioIRD/tot grainsTeitler, LoraCalculatedIRD Ratio = TIRD{split} / Grains tot{split}
28Accumulation rate, massMARmg/cm2/kaTeitler, LoraCalculatedMAR = SedRate × Dry Bulk Density (DBD). Note: because we did not have measured DBDs for our samples, in order to calculate MARs we used an average DBD of 0.8 g/cm³ (or, 800 mg/cm³)
29Accumulation rate, apparent massAMARmg/cm2/kaTeitler, LoraCalculatedAMAR = MAR × IRD ratio
30Sample, dry massSamp dmgTeitler, LoraCalculated
31Iceberg rafted debris, grains, per dry massIRD grains/dm#/gTeitler, LoraCalculatedTotal IRD {size fraction} = TIRD {split} × (2 *raised to the power of *#splits)
32Iceberg rafted debris, mass, minimumIRD m minmgTeitler, LoraCalculatedIRD min wt = IRD Ratio × Szfrac M × 1000
33Iceberg rafted debris, mass, per dry massIRD/dmmg/gTeitler, LoraCalculatedIRD mg/g = IRD min wt / Samp dM
34FragmentationFragm%Teitler, LoraAdopted from Hodell et al., 2001TN057-6-PC4 only
35RadiolariansRad%Teitler, LoraCalculatedRadiolarians / Total grains count {split} × 100
36ForaminiferaForam%Teitler, LoraCalculated(Foram plankt + Foram benth) / Total grains count {split} × 100
37Volcanic grains, total, in subsampleVolc grains tot subsample#Teitler, LoraCalculatedVolc lithics + Tephra
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
12810 data points

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