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Hayward, Bruce William; Sabaa, Ashwaq T; Grenfell, Hugh R (2004): (Appendix 1) Benthic foraminiferal abundance and diversities of ODP Site 181-1119. PANGAEA,, In supplement to: Hayward, BW et al. (2004): Benthic foraminifera and the Late Quaternary (last 150 ka) paleoceanographic and sedimentary history of the Bounty Trough, east of New Zealand. Palaeogeography, Palaeoclimatology, Palaeoecology, 211(1-2), 59-93,

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Latitude: -44.755533 * Longitude: 172.393383
Date/Time Start: 1998-08-05T00:00:00 * Date/Time End: 1998-08-26T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 52.02 m
181-1119 * Latitude: -44.755533 * Longitude: 172.393383 * Date/Time Start: 1998-08-05T00:00:00 * Date/Time End: 1998-08-26T00:00:00 * Elevation: -396.2 m * Penetration: 656.6 m * Recovery: 612.8 m * Location: South Pacific Ocean * Campaign: Leg181 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 70 cores; 656.6 m cored; 0 m drilled; 93.3% recovery
Depth is composite depth (mcd), using natural gamma and magnetic susceptibility (Carter et al., 1999, doi:10.2973/ The age model and identification of isotope stages is based on the cyclic sedimentation record, oxygen isotopes (Carter et al., 2004, doi:10.1016/S0025-3227(04)00017-9), and SST estimates from planktic foraminiferal faunas (Kate Wilson, unpub.). Further relevant data sets: Carter et al. (2004) doi:10.1594/PANGAEA.705263, Carter et al. (1999) doi:10.1594/PANGAEA.261020, doi:10.1594/PANGAEA.261021, doi:10.1594/PANGAEA.261022
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2AGEAgeka BPGeocode
3Sample code/labelSample labelHayward, Bruce WilliamDSDP/ODP/IODP sample designation
4Sample, optional label/labor noLab noHayward, Bruce William
5Marine isotopic stageMISHayward, Bruce William
6Size fraction < 0.063 mm, mud, silt+clay<63 µm%Hayward, Bruce WilliamGrain size, sieving
7Calcium carbonateCaCO3%Hayward, Bruce Williambased on reflectance measurements on Hole 1119C (Millwood et al., 2002, doi:10.2973/
8Foraminifera, plankticForam plankt%Hayward, Bruce WilliamCounting >63 µm fraction
9Fragmentation index, planktic foraminiferaFragm plankt foram%Hayward, Bruce WilliamCalculated (Le and Shackleton, 1992)
10Sea surface temperature, FebruarySST (2)°CHayward, Bruce WilliamModern analog technique (MAT)based on planktic foraminiferal faunal counts >150 µm, summer sea-surface
11Fishers alpha index of diversityFAIHayward, Bruce WilliamCalculated
12DiversityH(S)Hayward, Bruce WilliamCalculated
13Evenness of speciesEHayward, Bruce WilliamCalculated
14Foraminifera, benthicForam benth#/gHayward, Bruce WilliamCounting >63 µm fractiondry sediment
15Foraminifera, benthicForam benth#/gHayward, Bruce WilliamCounting >63 µm fractiondry sand fraction
16Accumulation rate, number of benthic foraminiferaBFAR#/cm2/kaHayward, Bruce WilliamCounting >63 µm fraction
17RadiolariansRad%Hayward, Bruce WilliamCounting >63 µm fraction
18Sedimentation rateSRcm/kaHayward, Bruce William
19Globigerina bulloides, δ18OG. bulloides δ18O‰ PDBHayward, Bruce Williambased on Carter et al. (2004)
20Globigerina bulloides, δ13CG. bulloides δ13C‰ PDBHayward, Bruce Williambased on Carter et al. (2004)
21Natural gamma rayNGRAPI unitsHayward, Bruce Williamfrom onboard measurements (Carter et al., 1999)
485 data points

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