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",
)

DataMeasurements(
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        measured_variables: [
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            "Latitude of event",
            "Longitude of event",
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            "δ13C",
            "δ18O",
            "δ13C",
            "δ18O",
            "δ13C",
            "δ18O",
            "δ13C",
            "δ18O",
            "δ13C",
            "δ18O",
            "δ13C",
            "δ18O",
            "δ13C",
            "δ18O",
            "δ13C",
            "δ18O",
            "δ13C",
            "δ18O",
        ],
        methods: [],
    },
)

DataMeasurements(
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        domain: Unspecified,
        station: None,
        measured_variables: [],
        methods: [],
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Origins: /Wissenschaft/PANGAEA

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

Region: Five-Ridge Tower Santiago-de-Chile-Platz Steinhorster Basin Nordfriesland 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

• PANGAEA (Herausgeberschaft)

Issued: 2020-03-18

Modified: 2022-02-23

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

Resources

• https://doi.pangaea.de/10.1594/PANGAEA.913661?format=textfile (TSV)

Status

Aktiv

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