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Carbon 13 isotopes reveal limited ocean circulation changes between interglacials of the last 800 ka

Description: We present a compilation of δ13C data to characterize the ocean circulation during the interglacials of the last 800 000 years. We selected 9 interglacials for which we have collected the available δ13C and δ18O values.

Global identifier:

Doi(
    "10.1594/PANGAEA.913661",
)

Types:
Measurements {
    domain: Unspecified,
    station: None,
    measured_variables: [
        "Event label",
        "Latitude of event",
        "Longitude of event",
        "Elevation of event",
        "δ13C",
        "δ18O",
        "δ13C",
        "δ18O",
        "δ13C",
        "δ18O",
        "δ13C",
        "δ18O",
        "δ13C",
        "δ18O",
        "δ13C",
        "δ18O",
        "δ13C",
        "δ18O",
        "δ13C",
        "δ18O",
        "δ13C",
        "δ18O",
    ],
    methods: [],
}
Dataset

Origins: /Wissenschaft/PANGAEA

Tags: Kohlenstoff ? Geografische Koordinaten ? Ozeanzirkulation ? Daten ? Meeresgewässer ? Zirkulation ? Carbon isotopes ? Interglacial ?

Region: Five-Ridge Tower Santiago-de-Chile-Platz Steinhorster Basin North Frisian Islands Walvis Ridge, Southeast Atlantic Ocean South Pacific Ocean South China Sea South Atlantic Ocean Indian Ocean Caribbean Sea/RIDGE Canarias Sea

Bounding boxes: -110.51833° .. 159.361° x -42.913616666667° .. 60.4035°

License: cc-by/4.0

Language: Englisch/English

Organisations

Issued: 2020-03-18

Modified: 2022-02-23

Time ranges: 1970-04-26 - 2004-10-30

Resources

Status

Quality score

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