Late Lutetian Thermal Maximum—Crossing a Thermal Threshold in Earth's Climate System?

Recognizing and deciphering transient global warming events triggered by massive release of carbon into Earth's ocean‐atmosphere climate system in the past are important for understanding climate under elevated pCO2 conditions. Here we present new high‐resolution geochemical records including b...

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Veröffentlicht in:	Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2018-01, Vol.19 (1), p.73-82
Hauptverfasser:	Westerhold, T., Röhl, U., Donner, B., Frederichs, T., Kordesch, W. E. C., Bohaty, S. M., Hodell, D. A., Laskar, J., Zeebe, R. E.
Format:	Artikel
Sprache:	eng
Schlagworte:	2°C warming of the deep ocean in the southern South Atlantic Astrophysics Atmosphere Carbon Carbon cycle Climate Climate change Climate system Dry season Earth Environmental changes Eocene Eocene transient (30 kyr) warming event at 41.52 Ma Foraminifera Geochemistry Global warming Late Lutetian Thermal Maximum (LLTM) occurs within magnetochron C19r LLTM coincidences with exceptionally high insolation Ocean warming Oceans Oxygen Oxygen isotopes Physics Positive feedback potential thermal threshold of Earth's climate system Sciences of the Universe Stable isotopes Temperature (air-sea)
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