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Hayward, Bruce W; 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 * 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 InvestigatorMethodComment
1DEPTH, sediment/rockDepthmGeocode
2AGEAgeka BPGeocode
3Sample code/labelSample labelHayward, Bruce WODP sample designation
4Sample, optional label/labor noLab noHayward, Bruce W
5Marine isotopic stageMISHayward, Bruce W
6Size fraction < 0.063 mm, mud, pelite, silt+clay<63 µm%Hayward, Bruce WGrain size, sieving
7Calcium carbonateCaCO3%Hayward, Bruce Wbased on reflectance measurements on Hole 1119C (Millwood et al., 2002, doi:10.2973/
8Foraminifera, plankticForam plankt%Hayward, Bruce WCounting >63 µm fraction
9Fragmentation index, planktic foraminiferaFragm plankt foram%Hayward, Bruce WCalculated (Le and Shackleton, 1992)
10Sea surface temperature, FebruarySST (2)°CHayward, Bruce WModern analog technique (MAT)based on planktic foraminiferal faunal counts >150 µm, summer sea-surface
11Fishers alpha index of diversityFAIHayward, Bruce WCalculated
12DiversityH(S)Hayward, Bruce WCalculated
13Evenness of speciesEHayward, Bruce WCalculated
14Foraminifera, benthicForam bent#/gHayward, Bruce WCounting >63 µm fractiondry sediment
15Foraminifera, benthicForam bent#/gHayward, Bruce WCounting >63 µm fractiondry sand fraction
16Accumulation rate, number of benthic foraminiferaBFAR#/cm2/kaHayward, Bruce WCounting >63 µm fraction
17RadiolariansRad%Hayward, Bruce WCounting >63 µm fraction
18Sedimentation rateSed ratecm/kaHayward, Bruce W
19Globigerina bulloides, δ18OG. bulloides δ18O‰ PDBHayward, Bruce Wbased on Carter et al. (2004)
20Globigerina bulloides, δ13CG. bulloides δ13C‰ PDBHayward, Bruce Wbased on Carter et al. (2004)
21Natural gamma rayGRAPI unitsHayward, Bruce Wfrom onboard measurements (Carter et al., 1999)
485 data points

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