Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Keigwin, Lloyd D (1982): (Table 2) Stable isotopes in foraminifers at DSDP Leg 78 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817079, Supplement to: Keigwin, LD (1982): Stable isotope stratigraphy and paleoceanography of Sites 502 and 503. In: Prell, WL; Gardner, JV; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 68, 445-453, https://doi.org/10.2973/dsdp.proc.68.119.1982

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Analyses of stable isotopes of monospecific planktonic foraminifers (G. quadrilobatus group) and monogeneric benthic foraminifers (Cibicidoides spp.) from late Neogene Atlantic Site 502 and Pacific Site 503 were conducted in order to determine the paleoceanographic changes resulting from the late Neogene uplift of the Panama Isthmus and from climatic cooling.
In general, results at each site are similar to those from previous studies for the late Miocene and late Pliocene time interval, documenting the late Miocene (6 Ma) shift in carbon isotopes and the inferred growth of permanent Northern Hemisphere continental ice sheets beginning about 3.2 Ma. Comparison of Atlantic-Pacific planktonic-benthic isotope data for four stratigraphic intervals (~6-8, ~5-6, ~3-5, and ~2-3 Ma) suggests that increasing isolation of Atlantic and Pacific low-latitude waters may be related to the emergence of the Panama Isthmus. The contrast between Atlantic and Pacific benthic foraminiferal d13C increased in two steps from 0.60 per mil to 1 per mil (the modern contrast) at about 6 Ma and 3 Ma. The first increase (0.15 per mil) may represent the end of previously limited deep-water communication between the Atlantic and Pacific at the present location of Panama. The second increase (0.25 per mil) may be due to increased production of North Atlantic Deep Water. This probably reflects the development of modern deep-sea circulation.
The d18O of planktonic foraminifers begins to increase in Atlantic Site 502 at 4.2 Ma and may reflect the increasing salinity of the North Atlantic Ocean arising from diminishing surface-water exchange across Panama. This increase is clearly shown by contrasting the d18O of Atlantic and Pacific planktonic foraminifers, as well as the d18O of planktonic and benthic foraminifers at Site 502. This inferred increase in surface-water salinity begins at the time of increasing provinciality of Atlantic and Pacific planktonic foraminifers.
Project(s):
Coverage:
Median Latitude: 8.518340 * Median Longitude: -85.882200 * South-bound Latitude: 4.050300 * West-bound Longitude: -95.638700 * North-bound Latitude: 11.491800 * East-bound Longitude: -79.378200
Date/Time Start: 1979-08-16T00:00:00 * Date/Time End: 1979-09-06T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 234.62 m
Event(s):
68-502A * Latitude: 11.491000 * Longitude: -79.379000 * Date/Time: 1979-08-16T00:00:00 * Elevation: -3051.0 m * Penetration: 214.8 m * Recovery: 178.6 m * Location: Caribbean Sea/RIDGE * Campaign: Leg68 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 62 cores; 195.1 m cored; 19.7 m drilled; 91.6 % recovery
68-502B * Latitude: 11.491800 * Longitude: -79.378200 * Date/Time: 1979-08-16T00:00:00 * Elevation: -3051.0 m * Penetration: 99.7 m * Recovery: 87.7 m * Location: Caribbean Sea/RIDGE * Campaign: Leg68 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 99.7 m cored; 0 m drilled; 88 % recovery
68-502C * Latitude: 11.491300 * Longitude: -79.378300 * Date/Time: 1979-08-16T00:00:00 * Elevation: -3051.0 m * Penetration: 228.7 m * Recovery: 110.8 m * Location: Caribbean Sea/RIDGE * Campaign: Leg68 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 35 cores; 125.3 m cored; 0 m drilled; 88.4 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Latitude of eventLatitude
3Longitude of eventLongitude
4Elevation of eventElevationm
5Sample code/labelSample labelKeigwin, Lloyd DDSDP/ODP/IODP sample designation
6DEPTH, sediment/rockDepth sedmGeocode – mbsf
7Cibicidoides wuellerstorfi, δ18OC. wuellerstorfi δ18O‰ PDBKeigwin, Lloyd Dsee reference(s)
8Cibicidoides wuellerstorfi, δ13CC. wuellerstorfi δ13C‰ PDBKeigwin, Lloyd Dsee reference(s)
9Cibicidoides kullenbergi, δ18OC. kullenbergi δ18O‰ PDBKeigwin, Lloyd Dsee reference(s)
10Cibicidoides kullenbergi, δ13CC. kullenbergi δ13C‰ PDBKeigwin, Lloyd Dsee reference(s)
11Globigerinoides quadrilobatus, δ18OG. quadril δ18O‰ PDBKeigwin, Lloyd Dsee reference(s)
12Globigerinoides quadrilobatus, δ13CG. quadril δ13C‰ PDBKeigwin, Lloyd Dsee reference(s)
13Oridorsalis tener, δ18OO. tener δ18O‰ PDBKeigwin, Lloyd Dsee reference(s)
14Oridorsalis tener, δ13CO. tener δ13C‰ PDBKeigwin, Lloyd Dsee reference(s)
Size:
699 data points

Download Data

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

View dataset as HTML