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  • Data  (3)
  • 121-758A; Catapsydrax dissimilis, δ13C; Catapsydrax dissimilis, δ18O; Catapsydrax spp., δ13C; Catapsydrax spp., δ18O; Catapsydrax unicavus, δ13C; Catapsydrax unicavus, δ18O; Comment; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Fohsella kugleri, δ13C; Fohsella kugleri, δ18O; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Foraminifera, planktic δ13C; Foraminifera, planktic δ18O; Globigerina binaiensis, δ13C; Globigerina binaiensis, δ18O; Globigerina euapertura, δ13C; Globigerina euapertura, δ18O; Globigerina galavisi, δ13C; Globigerina galavisi, δ18O; Globigerina sellii, δ13C; Globigerina sellii, δ18O; Globigerina tripartita, δ13C; Globigerina tripartita, δ18O; Globorotaloides suteri, δ13C; Globorotaloides suteri, δ18O; Indian Ocean; Jenkinsella spp., δ13C; Jenkinsella spp., δ18O; Joides Resolution; Leg121; Mass spectrometer Finnigan MAT 251; Ocean Drilling Program; ODP; ORDINAL NUMBER; Sample code/label  (1)
  • 14-137; 80-551; Counting, foraminifera, planktic; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Glomar Challenger; Guembelitria cenomana, δ13C; Guembelitria cenomana, δ18O; Hedbergella delrioensis, δ13C; Hedbergella delrioensis, δ18O; Heterohelix moremani; Heterohelix moremani, δ13C; Heterohelix moremani, δ18O; Isotope ratio mass spectrometry; Leg14; Leg80; North Atlantic/ESCARPMENT; North Atlantic/HILL; ORDINAL NUMBER; Praeglobotruncana spp., δ13C; Praeglobotruncana spp., δ18O; Rotalipora cushmani, δ13C; Rotalipora cushmani, δ18O; Rotalipora gandolfii, δ13C; Rotalipora gandolfii, δ18O; Sample code/label; δ13C, carbonate; δ18O, carbonate  (1)
  • 93-603B; 93-604; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Globigerinoides obliquus, δ13C; Globigerinoides obliquus, δ18O; Globigerinoides ruber, δ13C; Globigerinoides ruber, δ18O; Globorotalia inflata, δ13C; Globorotalia inflata, δ18O; Glomar Challenger; Leg93; Mass spectrometer Finnigan MAT 251; North Atlantic/CONT RISE; Sample code/label; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O  (1)
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  • Data  (3)
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  • 1
    facet.materialart.
    Unknown
    (Table 2) Oxygen and carbon isotope composition of planktonic foraminiferal species from DSDP Holes 93-603B and 93-604, and one benthic species from Hole 93-604
    PANGAEA
    In:  Supplement to: Ganssen, Gerald M (1987): Late Cenozoic stable isotopic stratigraphy, Deep Sea Drilling Project Sites 603 and 604, Northeast American continental rise. In: van Hinte, JE; Wise, SW Jr; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 93, 997-1002, https://doi.org/10.2973/dsdp.proc.93.139.1987
    Details
    Publication Date: 2023-06-27
    Description: Holes 603C and 604 of DSDP Leg 93 were drilled on the western Atlantic continental rise at water depths of 4633 m and 2364 m, respectively. In Hole 603C, a nearly continuous, undisturbed, and complete section of Pliocene and lower Pleistocene sediments was recovered by hydraulic piston coring; in Hole 604, a section of uppermost Miocene to Pleistocene sediments was incompletely recovered by rotary coring. In order to reconstruct the Pliocene and Pleistocene history of isotopic variations, 139 oxygen and carbon isotope values were determined for planktonic and monospecific benthic foraminifer samples from these holes. Large parts of the Pleistocene history could not, however, be documented because sample intervals were large and sediments at Site 604 were redeposited. Time correlation is based on magnetostratigraphic (Hole 603C) and micropaleontologic (Hole 603C, Site 604) interpretation. Stable isotope analyses were carried out on the planktonic foraminiferal species Globigerinoides ruber, G. obliquus, and Globorotalia inflata from Hole 603C (48 analyses) and from Site 604 (48 analyses); at Site 604, the benthic foraminifer Uvigerina peregrina (43 analyses) was also studied through the section. Age calibration for Hole 603C is based on the magnetostratigraphy of Canninga et al. (1987; doi:10.2973/dsdp.proc.93.130.1987), which uses the time scale of Lowrie and Alvarez (1981).
    Keywords: 93-603B; 93-604; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Globigerinoides obliquus, δ13C; Globigerinoides obliquus, δ18O; Globigerinoides ruber, δ13C; Globigerinoides ruber, δ18O; Globorotalia inflata, δ13C; Globorotalia inflata, δ18O; Glomar Challenger; Leg93; Mass spectrometer Finnigan MAT 251; North Atlantic/CONT RISE; Sample code/label; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 384 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 2
    facet.materialart.
    Unknown
    Stable carbon and oxygen isotope record of Cretaceous planktonic foraminifera from DSDP (Table 1) (1998)
    PANGAEA
    In:  Supplement to: Nederbragt, Alexandra J; Erlich, Robert N; Fouke, Bruce W; Ganssen, Gerald M (1998): Palaeoecology of the biserial planktonic foraminifer Heterohelix moremani (Cushman) in the late Albian to middle Turonian Circum-North Atlantic. Palaeogeography, Palaeoclimatology, Palaeoecology, 144(1-2), 115-133, https://doi.org/10.1016/S0031-0182(98)00089-3
    Details
    Publication Date: 2023-07-11
    Description: The Cretaceous Heterohelix moremani (Cushman) was the only biserial planktonic foraminiferal species from its first appearance in the late Albian up to the Cenomanian/Turonian boundary. Within that time, it increased gradually in abundance relative to other planktonic foraminifera in five Circum-North Atlantic sections. It is generally rare in upper Albian sediments, common in most of the Cenomanian and very abundant in sediments representing the latest Cenomanian Oceanic Anoxic Event. Short-term variations on the overall abundance trend correlate with positive excursions in the bulk carbonate delta13C record. Maximum rain rates of H. moremani during OAE2 show that this species was an opportunist that did well in extreme conditions, but its overall distribution indicates that it is not necessarily a marker for very high palaeoproductivity environments. Stable oxygen and carbon isotope measurements on foraminiferal species indicate that H. moremani was a surface water dweller at least in part of its geographic range, but incorporated 13C out of equilibrium with ambient seawater. It is depleted in delta13C relative to other planktonic foraminifera, which is attributed to vital effects related to its opportunistic character.
    Keywords: 14-137; 80-551; Counting, foraminifera, planktic; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Glomar Challenger; Guembelitria cenomana, δ13C; Guembelitria cenomana, δ18O; Hedbergella delrioensis, δ13C; Hedbergella delrioensis, δ18O; Heterohelix moremani; Heterohelix moremani, δ13C; Heterohelix moremani, δ18O; Isotope ratio mass spectrometry; Leg14; Leg80; North Atlantic/ESCARPMENT; North Atlantic/HILL; ORDINAL NUMBER; Praeglobotruncana spp., δ13C; Praeglobotruncana spp., δ18O; Rotalipora cushmani, δ13C; Rotalipora cushmani, δ18O; Rotalipora gandolfii, δ13C; Rotalipora gandolfii, δ18O; Sample code/label; δ13C, carbonate; δ18O, carbonate
    Type: Dataset
    Format: text/tab-separated-values, 58 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
  • 3
    facet.materialart.
    Unknown
    Stable carbon and oxygen istotope ratios of Oligocene foraminifera from ODP Hole 121-758A of the northern Ninetyeast Ridge, Indian Ocean (Appendix 1) (1995)
    PANGAEA
    In:  Supplement to: van Eijden, AJM; Ganssen, Gerald M (1995): An Oligocene multi-species foraminiferal oxygen and carbon isotope record from ODP Hole 758A (Indian Ocean): paleoceanographic and paleo-ecologic implications. Marine Micropaleontology, 25(1), 47-65, https://doi.org/10.1016/0377-8398(94)00028-L
    Details
    Publication Date: 2024-01-09
    Description: An Oligocene-basal Miocene (Zones P19-P22/N4) oxygen and carbon isotope stratigraphy is presented based on mixed benthic foraminiferal faunas and different species of planktic foraminifers from Eastem Indian Ocean ODP Hole 758A. Lack of covariance in planktic and benthic delta18O ratios indicates that many Oligocene sea level fluctuations, including the major fall at 30 Ma, are not of glacio-eustatic origin. Delta18O values suggest that test morphology is a poor indicator of preferred depth habitat of Oligocene planktic foraminifers. Also, some groups show considerable shifts in preferred depth habitat. Reconstructed surface water temperature was nearly constant during the investigated period, but even assuming a large Antarctic icecap, values are unrealistically low, 18°-20°C. Most likely, water masses with markedly different oxygen isotopic composition existed, this poses great problems for quantitative temperature reconstructions. Planktic foraminiferal species show similar delta13C ratios, indicating well-mixed surface waters. This contrasts with the strong oxygen isotopic gradient, which suggests well-stratified surface waters. During the Oligocene the difference in delta13C ratio between the average ratio of planktic foraminiferal species and the benthic foraminifers (Delta delta13C P-B') shows an inverse relation with the known circulation intensity record and thus with productivity. This Delta delta13C pattern is interpreted as being caused by the presence of younger bottom waters at this site during periods with lower temperatures and/or larger Antarctic ice sheets.
    Keywords: 121-758A; Catapsydrax dissimilis, δ13C; Catapsydrax dissimilis, δ18O; Catapsydrax spp., δ13C; Catapsydrax spp., δ18O; Catapsydrax unicavus, δ13C; Catapsydrax unicavus, δ18O; Comment; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Fohsella kugleri, δ13C; Fohsella kugleri, δ18O; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Foraminifera, planktic δ13C; Foraminifera, planktic δ18O; Globigerina binaiensis, δ13C; Globigerina binaiensis, δ18O; Globigerina euapertura, δ13C; Globigerina euapertura, δ18O; Globigerina galavisi, δ13C; Globigerina galavisi, δ18O; Globigerina sellii, δ13C; Globigerina sellii, δ18O; Globigerina tripartita, δ13C; Globigerina tripartita, δ18O; Globorotaloides suteri, δ13C; Globorotaloides suteri, δ18O; Indian Ocean; Jenkinsella spp., δ13C; Jenkinsella spp., δ18O; Joides Resolution; Leg121; Mass spectrometer Finnigan MAT 251; Ocean Drilling Program; ODP; ORDINAL NUMBER; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 418 data points
    Location Call Number Expected Availability
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    DATA PANGAEA
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