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Powell, Ross; Hambrey, Mike J; Krissek, Lawrence A (1998): Description of lithofacies associations and their interpreted settings from sequences of sediment core CRP-1 (Table 2) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.433089, Supplement to: Powell, R et al. (1998): Quaternary and Miocene glacial and climatic history of the Cape Roberts drillsite region, Antarctica. Terra Antartica, 5(3), 341-351, hdl:10013/epic.28313.d001

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Abstract:
Cape Roberts Project drillcore 1 was obtained from Roberts Ridge, a sea-floor high located at 77°S, 16 km offshore from Cape Roberts in western McMurdo Sound, Antarctica. The recovered core is about 147 m long with the upper 43.15 metres below the sea floor (revised figure) being dated as Quarternary and the older part of the sequence being Miocene. The core includes nine facies: sandy diamict, muddy diamict, gravel/conglomerate, mud(stone), clay(stone) and carbonate. These facies occure in associations that are repeated in particulare sequences throughout the core, and are interpreted as representing different depositional environments through time. Seven lithofacies associations are interpreted as representing offshore shelf, ice protected/below wave-base; prodeltaic/offshore shelf; delta front/sandy shelf; ice system; subglacial till/rainout diamict/debris flow diamicts singly or in combination; and a carbonate-rich shelf bank. The facies associations are used to infer that the Quaternary section represents deposition on a polar shelf with perhaps two or three glacial fluctuations. The Quaternary carbonate unit indicates a period of ice sheet retreat, but local glacial activity may have increased with an increase in costal precipitation. The Miocene section represents polythermal glacial systems. The older Miocene section is glacially dominated whereas the younger section is much less so. The glacially dominated section may provide evidence for a major glacial advance thar resulted un a low stand of global eustatic sea level at that time. After the low stand, eustatic sea level was gradually rising during deposition of the younger section dominated more by non-glacial processes.
Project(s):
Coverage:
Latitude: -77.007580 * Longitude: 163.755080
Date/Time Start: 1997-10-17T01:30:00 * Date/Time End: 1997-10-24T02:00:00
Minimum DEPTH, sediment/rock: 20.565 m * Maximum DEPTH, sediment/rock: 148.595 m
Event(s):
CRP-1 (16 km ENE Cape Roberts) * Latitude: -77.007580 * Longitude: 163.755080 * Date/Time Start: 1997-10-17T01:30:00 * Date/Time End: 1997-10-24T02:00:00 * Elevation: -153.5 m * Penetration: 132.06 m * Recovery: 113.32 m * Location: off Cape Roberts, Ross Sea, Antarctica * Campaign: CRP-1 * Basis: Sampling/drilling ice * Method/Device: Core wireline system (CWS) * Comment: sea ice thickness: 1.60 m, recovery 86 %. Age and lithology of oldest strata: 22-24 Ma; mudstone with scattered pebbles.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Depth, top/minDepth topmPowell, Ross
Depth, bottom/maxDepth botmPowell, Ross
Facies name/codeFaciesPowell, Ross
Lithology/composition/faciesLithologyPowell, Ross
EnvironmentEnvironmentPowell, Ross
Size:
157 data points

Data

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Depth sed [m]

Depth top [m]

Depth bot [m]

Facies

Lithology

Environment
20.56519.1322.00Sandy diamicts (Structureless diamict)Rainout (?and subglacial), ice contact and ice proximalGlacial shelf deposition, rainout/(?) subglacial
23.27522.0024.55No core
24.81524.5525.08Sandy diamicts (Rainout diamict graded up from sandy mud below)Rainout , ice contact and ice proximalGlacial shelf deposition
25.75525.0826.43Muds (Suspension deposited mud, ?drilling disturbed?)Offshore shelf, ice protected/below wave-base, paraglacial
27.96026.4329.49Graded sands (Marine current-deposited sands and sandy turbidites)Delta front/sandy shelf, below wave-base, non-glacial(?)Glacial shelf deposition during glacial retreat
30.69029.4931.89Sandy diamicts+graded sands (Sharp and graded contacts, diamict-diamict, diamict-sandIce-contact, ice proximal mass flow, and rainout systemsGlacial shelf deposition at and near grounding-line
32.85531.8933.82Fossiliferous siliciclastics+calcareous sandy mud+muds+sandy diamicts+graded sands (Coquina, calcareous mud, diamict, diamict-sand)Carbonate shelfDeposition on shelf bank with some influence of iceberg rafting
38.68533.8243.55Sandy diamicts+muds+gravels (Diamicts with graded contacts within and with muds, Ionestone horizons)Rainout with local subglacial (?), ice contact and ice proximalGlacial shelf deposition, (?) minor glacial fluctuation, (?) more distal upward
46.89043.5550.23Stratified sands+graded sands (Marine current-deposited sands and sandy turbidites)Delta front/sandy shelf, below wave-base/(?) ice protected, non-glacial/(?)paraglacial
51.96550.2353.70Muds (Suspension settling deposits)Poorly constrained. Offshore shelf, below wave-base, non-glacial(?)Offshore sedimentation in general coarsening-up progradation during glacial retreat phase
54.77553.7055.85Graded sands+sandy diamicts+muds (Sandy turbidites, debris flow diamicts, traction sands, cyclo-pels, Ionestone layers)Ice contact and ice proximal mass flow and submarine fluvial efflux systemIce contact grounding-line fan system
57.82555.8559.80Muds+breccias+graded sands (Suspension settling deposits and very low density gravity flow deposits)Prodeltaic/offshore shelf, below wave-base, non-glacialOffshore sedimentation in glacial retreat phase
60.68559.8061.57Graded sands+muds+gravels (Stacked sandy turbidites, rare debris flow diamicts, Ionestones)Ice-contact and ice proximal mass flow and submarine fluvial efflux system
62.38561.5763.20Sandy diamicts+graded sands+gravels (Debris flow diamicts, subglacial till, rare sandy turbidites)Ice-contact and ice proximal mass flow system, some sub-glacial deposition(?)Ice contact morainal bank and probank and grounding-line fan system
66.35563.2069.51Graded sands+stratified sands+muds (Sandy turbidites and marine current-deposited (+aeolian mix?) sands)Delta front/sandy shelf, non-glacial
69.89569.5170.28Muds+clays+breccias (Suspension settling deposits and very low density gravity flow deposits)Offshore shelf (?prodelta), ice protected/below wave-base, paraglacial/(?)non-glacial
72.96570.2875.65Graded sands+stratified sands+muds (Gravity flow and traction (+aeolian mix?) deposits with rare Ionestones)Delta front/sandy shelf, ice-protected/below wave-base, paraglacialShelf progradation with glacial influence in last stages, then glacial retreat with continued shelf
77.17575.6578.70Clays+muds (Suspension setting deposits with rare lonestones)Offshore shelf, ice protected/below wave-base, paraglacial
79.93078.7081.16Sandy diamicts+graded sands+gravels+breccias (Debris flow diamicts and (?)subglacial till)Ice contact and ice proximal mass flow and submarine fluvial efflux system, (?)sub-glacial, reworked lags and redeposited flowsIce contact grounding-line fan and morainal bank and then glacial over-riding; final stage - shallow water reworking
81.76581.1682.37Muds (Suspension settling deposits with rare Ionestones)Offshore shelf, ice protected/below wave-base, paraglacial
83.21582.3784.06Graded sands+muds+stratified sands(+B) (Gravity flow and traction deposits with rare Ionestones)Delta front/sandy shelf, paraglacial
84.95584.0685.85Muds (Suspension settling deposits with rare Ionestones)Offshore shelf, ice protected/below wave-base, paraglacialNearshore to off-shore paraglacial delta/shelf - two cycles
89.02085.8592.19Graded sands+stratified sands (Gravity flow and traction deposits with rare Ionestones)Delta front/sandy shelf, paraglacial
97.30592.19102.42Muds+graded sands (Suspension settling deposits with clasts as Ionestones and in horizons, low density gravity flow deposits)Prodeltaic/offshore shelf, medial glacimarine to paraglacialMedial glacimarine with glacial retreat and then shoreline progradation at start of sequence above
102.915102.42103.41Graded sands+muds (Stacked low density gravity flow deposits, Ionestones)Delta front/sandy shelf, glacial
106.085103.41108.76Sandy diamicts+graded sands (Debris flow diamicts and (?)subglacial till)Ice contact and ice proximal mass flow systemGrounding-line fan, then morainal bank and pro-bank and then delta
109.380108.38110.38Graded sands+muds (Stacked sandy turbidites, Ionestones and dropstones, cyclopels and cyclopsams)Ice contact and ice proximal mass flow and submarine fluvial efflux system
112.240110.38114.10Graded sands+stratified sands+muds (Sandy turbidites and marine current-depo-sited sands, suspension settling deposits)Delta front/prodelta/shelf, below wave base, non-glacialNearshore to offshore non-glacial delta/shelf - two cycles
116.690114.10119.28Graded sands+sandy diamicts+muds (Stacked debris flow diamicts, sandy turbidites, ice-rafted debris as lonestones and pavements, soft sediment deformation and fluid escape)Ice contact and ice proximal mass flow and submarine fluvial efflux system
126.965119.28134.65muddy diamicts+sandy diamicts+graded sands+muds (Debris flow diamicts with thin low density gravity flow deposits, graded/amalgamated contacts, soft sediment deformation)Ice-contact and ice proximal mass flow systemIce contact morainal bank and probank then grounding-line fan or delta
137.875134.65141.10muddy diamicts (Structureless diamict - till or rainout)Subglacial or rainout, ice contact and ice proximal
141.725141.10142.35Graded sands+muds (Sandy turbidites, suspension settling deposits)Prodeltaic/offshore shelf, medial glacimarine
144.445142.35146.54Clays+muds (Suspension setting deposits with rare clasts as lonestones, low density gravity flow deposits)Offshore shelf, ice protected/below wave-base, paraglacial
146.865146.54147.19Muds+clays+graded sands (Suspension setting deposits, low density gravity flow deposits)Prodeltaic/offshore shelf, distal glacimarineDeltaic/shelf below wave base, from medial to distal glacimarine to paraglacial/(?) nonglacial to medial glacimarine upward, showing glacial retreat then advance
148.595147.19150.00Graded sands (Sandy turbidites) down to end of coreDelta front/sandy, medial glacimarine