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Wilson, Gary S; Bohaty, Steven M; Fielding, Christopher R; Florindo, Fabio; Hannah, Mike J; Harwood, David M; McIntosh, W C; Naish, Tim R; Roberts, Andrew P; Sagnotti, Leonardo; Scherer, Reed P; Strong, C Percy; Versub, K L; Villa, Giuliana; Watkins, David K; Webb, Peter-Noel; Woolfe, Ken (2000): Chronostratigraphy of sediment core CRP-2/2A (Table 1) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.189249, Supplement to: Wilson, GS et al. (2000): Chronostratigraphy of CRP-2/2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(4), 647-654, hdl:10013/epic.28244.d001

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Abstract:
The 624.15 m glaciomarine sedimentary succession recovered in the CRP-2/2A drillcore comprises lower Oligocene (<c. 31 Ma) to lower Miocene (18.5 Ma) strata that are overlain by a thin succession of Pliocene and Pleistocene strata. The age model for the CRP-2/2A drillhole, as presented in this paper, is based on combined microfossil biostratigraphy. 40Ar/39Ar age on volcanic material, 87Sr/86Sr analyses on mollusc shells, and correlation of a magnetic polarity zonation to the magnetic polarity time scale (MPTS). Between 25.92 and 109.05 metres below sea floor (mbsf), several alternative correlations to the MPTS are possible, all of which suggest that sediment accumulation rates averaged ~180 m/m.y. between unconformities, although actual sedimentation rates may have been higher. Between 109.05 and 306.65 mbsf, the age model is straightforward and average sedimentation rates were much higher (>1000 m/m.y.). Between 306.65 mbsf and the bottom of the drillcore (624.15 mbsf), fewer datums are available to constrain the age model and unique correlation with the MPTS is not possible, although high average sediment accumulation rates are likely. A significant unconformity is identified at 306.65 mbsf, which may represent as much as 5 m.y. of missing time. Additional unconformities at 25.92 and 130.27 mbsf account for c. 16 and 2.5 m.y. of missing time, respectively. The Oligocene-lower Miocene interval documented in the CRP-2/2A drillcore spans about 13 million years, however, it is possible that more time is missing in sequence-bounding unconformities than is represented in the stratigraphic record recovered in the CRP-2/2A drillcore.
Project(s):
Coverage:
Latitude: -77.005980 * Longitude: 163.719450
Date/Time Start: 1998-10-16T07:30:00 * Date/Time End: 1998-11-25T14:20:00
Minimum DEPTH, sediment/rock: 36.020 m * Maximum DEPTH, sediment/rock: 624.150 m
Event(s):
CRP-2A (14.2 km at 096° true from Cape Roberts) * Latitude: -77.005980 * Longitude: 163.719450 * Date/Time Start: 1998-10-16T07:30:00 * Date/Time End: 1998-11-25T14:20:00 * Elevation: -177.9 m * Recovery: 624 m * Location: off Cape Roberts, Ross Sea, Antarctica * Campaign: CRP-2 * Basis: Sampling/drilling from ice * Method/Device: Core wireline system (CWS) * Comment: 921 m at 284° from CRP-1. Sea-ice thickness: 2.0 m (1 Oct) to 2.2 m (23 Nov). Sea riser embedded to 13.03 mbsf. Lateral ice movement: 9.87 m to east from 17 Oct to 23 Nov. HQ core to 199.31 mbsf. NQ core to 624.15 mbsf. 13.03 to 45.97 mbsf, 11.29 m (34%) partially following CRP-2. 45.07 to 624.15 mbsf, 548.67 m (95%) new hole. Deepest core-lithology: hard sandy siltstone. Deepest core-age: earliest Oligocene (ca. 33 Ma on diatoms, nannofossils and dinoflagellates)
Size:
199 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth sed [m]

Depth top [m]

Depth bot [m]

Sample label

Dated material

Age dated [ka]

Age e - [ka -]

Age e + [ka +]

Comm
36.020A1Basaltic Clast19180260260
36.25536.2436.27S1Solitary coral (in situ)18620220210
41.83036.2547.41D1FO Thalassiosira praefraga complex20300(C6r)
54.96054.9454.98S2Bivalve fragment (provenance uncertain)20350380420
54.96054.9454.98S2Bivalve fragment (provenance uncertain)20290640550
112.500111.00114.00A2Pumice214405050
125.925125.92125.93A3Trachyte Clast22560290290
126.555126.55126.56S3Pectinid fragment (provenance uncertain)22240390390
144.440Nf1LO Dictycoccites bisectus23900(C6Cn.2r)
193.000A4Pumice23980130130
194.890194.87194.91S4Bivalve (in situ)24520630660
198.745198.74198.75S5Bivalve fragment (provenance uncertain)24100350360
246.985246.97247.00S6Bivalve (in situ)24020350350
247.690247.67247.71S7Bivalve fragment (provenance uncertain)24810340340
248.140236.26260.02D2LO Lisitzinia ornata24100(C6Cr)
280.030A5Pumice242206060
294.220A6Trachyte Clast24980170170
408.830405.39412.27D3LO Eurossia irregularis2700027 to 29 Ma (C9 - C10)
408.830405.39412.27D4LO Pyxilla reticulata30100(C11r)
412.250Nf2LO Chiasmolithus altus26100(C8)
439.610437.37441.85D5LO Rhizosolenia antarctica29800(C11n.2n)
442.880441.87443.89D6LO Rhizosolenia oligocaenica29600(C11n.1r)
444.430443.90444.96D7LO Asterolampra punctifera27000(C9n)
445.045445.03445.06S8Modiolid fragment (in situ)29410520500
460.655460.64460.67S9Modiolid fragment (in situ)29550520540
463.370463.36463.38S10Modiolid fragment (in situ)29890510520
483.165483.15483.18S11Modiolid fragment (in situ)30670450480
483.165483.15483.18S11Modiolid fragment (in situ)30330480500
483.165483.15483.18S11Modiolid fragment (in situ)30390470510
554.220543.81564.63D8FO Cavitatus jouseanus30900(C12n)
564.670D9CIROS-1 <Assemblage B> absent<33000(C13n)
564.670D9LO Hemiaulus characteristicus absent<33000(C13n)
624.150MP1<Transantarctic assemblage> absent(<C13n to C15n)