Biolzi, Milena (1983): Stable oxygen and carbon isotope ratios of foraminifera from Oligocene to Miocene sediments of DSDP Hole 39-354 from Ceara Rise, West Altlantic (Table 1) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.690399, Supplement to: Biolzi, M (1983): Stable isotopic study of Oligocene-Miocene sediments from DSDP Site 354, Equatorial Atlantic. Marine Micropaleontology, 8(2), 121-139, https://doi.org/10.1016/0377-8398(83)90008-7
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Abstract:
The oxygen- and carbon-isotope compositions of planktic and benthic foraminifera and calcareous nannofossils from Middle Oligocene-Early Miocene Equatorial Atlantic sediments (DSDP Site 354) indicate two important paleoceanographic changes, in the Late Oligocene (foraminiferal Zone P.21) and in the Early Miocene (foraminiferal Zone N.5). The first change, reflected by a delta18O increase of 1.45‰ in Globigerina venezuelana, affected only intermediate pelagic and not surface, deep or bottom waters. The second change affected surface and intermediate waters, whereas deep and bottom waters showed only minor fluctuations. In the case of the former the isotope effect of the moderate ice accumulation on the Antarctic continent is amplified in the Equatorial Atlantic by changes in the circulation pattern. The latter paleoceanographic change, reflected by a significant increase in 18O in both planktic and benthic forms (about 1.0‰ and 0.5‰, respectively), may have been caused by ice volume increase and temperature decrease. Both oxygen- and carbon-isotope compositions indicate a marked depth-habitat stratification for planktic foraminifera and calcareous nannofossils. Three different dwelling groups are recognized: shallow Globigerinoides, Globoquadrina dehiscens, Globorotalia mayeri and nannofossils; intermediate Globigerina venezuelana; and deep Catapsydrax dissimilis. The comparison of foraminifera and calcareous nannofossils suggests that the isotopic compositions of nannofossils are generally controlled by the same parameters which control the isotopic composition of shallow-dwelling foraminifera, but the former are more enriched in 18O.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 5.899200 * Longitude: -44.196300
Date/Time Start: 1974-10-27T00:00:00 * Date/Time End: 1974-10-27T00:00:00
Minimum ORDINAL NUMBER: 1 * Maximum ORDINAL NUMBER: 29
Event(s):
39-354 * Latitude: 5.899200 * Longitude: -44.196300 * Date/Time: 1974-10-27T00:00:00 * Elevation: -4045.0 m * Penetration: 900 m * Recovery: 119 m * Location: North Atlantic/CONT RISE * Campaign: Leg39 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 19 cores; 211 m cored; 0 m drilled; 56.4 % recovery
Comment:
Analyzed specimens: planktic foraminifera 20-30, benthic foraminifera 5-12
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | ORDINAL NUMBER | Ord No | Geocode | |||
2 | Sample code/label | Sample label | Biolzi, Milena | DSDP/ODP/IODP sample designation | ||
3 | Planktic foraminifera zone | Plank foram zone | Biolzi, Milena | Zonation of Blow (1969) | ||
4 | Globigerina venezuelana, δ18O | G. venezuelana δ18O | ‰ PDB | Biolzi, Milena | ||
5 | Globigerina venezuelana, δ13C | G. venezuelana δ13C | ‰ PDB | Biolzi, Milena | ||
6 | Catapsydrax dissimilis, δ18O | C. dissimilis δ18O | ‰ PDB | Biolzi, Milena | ||
7 | Catapsydrax dissimilis, δ13C | C. dissimilis δ13C | ‰ PDB | Biolzi, Milena | ||
8 | Globigerinoides ruber, δ18O | G. ruber δ18O | ‰ PDB | Biolzi, Milena | ||
9 | Globigerinoides ruber, δ13C | G. ruber δ13C | ‰ PDB | Biolzi, Milena | ||
10 | Globigerinoides trilobus, δ18O | G. trilobus δ18O | ‰ PDB | Biolzi, Milena | ||
11 | Globigerinoides trilobus, δ13C | G. trilobus δ13C | ‰ PDB | Biolzi, Milena | ||
12 | Globoquadrina dehiscens, δ18O | G. dehiscens δ18O | ‰ PDB | Biolzi, Milena | ||
13 | Globoquadrina dehiscens, δ13C | G. dehiscens δ13C | ‰ PDB | Biolzi, Milena | ||
14 | Globoquadrina globularis, δ18O | G. globularis δ18O | ‰ PDB | Biolzi, Milena | ||
15 | Globoquadrina globularis, δ13C | G. globularis δ13C | ‰ PDB | Biolzi, Milena | ||
16 | Globorotalia mayeri, δ18O | G. mayeri δ18O | ‰ PDB | Biolzi, Milena | ||
17 | Globorotalia mayeri, δ13C | G. mayeri δ13C | ‰ PDB | Biolzi, Milena | ||
18 | Globorotalia kugleri, δ18O | G. kugleri δ18O | ‰ PDB | Biolzi, Milena | ||
19 | Globorotalia kugleri, δ13C | G. kugleri δ13C | ‰ PDB | Biolzi, Milena | ||
20 | Globorotalia opima opima, δ18O | G. opima opima δ18O | ‰ PDB | Biolzi, Milena | ||
21 | Globorotalia opima opima, δ13C | G. opima opima δ13C | ‰ PDB | Biolzi, Milena | ||
22 | δ18O, carbonate | δ18O carb | ‰ PDB | Biolzi, Milena | mixed nannofossil, < 28 µm | |
23 | δ13C, carbonate | δ13C carb | ‰ PDB | Biolzi, Milena | mixed nannofossil, < 28 µm | |
24 | Cibicidoides pseudoungerianus, δ18O | C. pseudoungerianus δ18O | ‰ PDB | Biolzi, Milena | for correction disequilibrium (difference to Uvigerina spp.) +0.40 per mil (Boersma and Shackleton, 1977a, b) | |
25 | Cibicidoides pseudoungerianus, δ13C | C. pseudoungerianus δ13C | ‰ PDB | Biolzi, Milena | for correction disequilibrium (difference to Uvigerina spp.) -0.76 per mil (N.J. Shackleton, pers. comm. 1982) | |
26 | Globocassidulina subglobosa, δ18O | G. subglobosa δ18O | ‰ PDB | Biolzi, Milena | for correction disequilibrium (difference to Uvigerina spp.) +0.10 per mil (Boersma and Shackleton, 1977a, b) | |
27 | Globocassidulina subglobosa, δ13C | G. subglobosa δ13C | ‰ PDB | Biolzi, Milena | ||
28 | Oridorsalis umbonatus, δ18O | O. umbonatus δ18O | ‰ PDB | Biolzi, Milena | ||
29 | Oridorsalis umbonatus, δ13C | O. umbonatus δ13C | ‰ PDB | Biolzi, Milena | ||
30 | Stilostomella spp., δ18O | Stilostomella spp. δ18O | ‰ PDB | Biolzi, Milena | ||
31 | Stilostomella spp., δ13C | Stilostomella spp. δ13C | ‰ PDB | Biolzi, Milena | ||
32 | Foraminifera, benthic δ18O | Foram benth δ18O | ‰ PDB | Biolzi, Milena | ||
33 | Foraminifera, benthic δ13C | Foram benth δ13C | ‰ PDB | Biolzi, Milena |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
415 data points