Palaeoclimate is the reconstruction and study of past climate states on Earth and other planets. Climate parameters such as precipitation, temperature, wind strength, and patterns of interannual climate variability are frequently estimated from proxies in ice and sediment cores, tree rings, cave deposits and historical records. These are assessed in numerical models.


Latest Research and Reviews

News and Comment

  • News and Views |

    Extreme temperature swings and deteriorating environments are perhaps what killed most life in the end-Permian extinction, suggest climate model simulations. Siberian Traps volcanism probably triggered the events.

    • Ying Cui
    Nature Geoscience 11, 889–890
  • Editorial |

    Fifty years of international ocean drilling have brought enormous insights into the workings of our planet. Incorporating young investigators’ ideas, cooperating internationally and sharing data and samples have been key to this success.

  • News and Views |

    Ice buried deep within the ice sheet on Antarctica preserves clues to past climatic change dating back more than a million years. A recent workshop discussed the challenges — and hopes — of drilling to these buried treasures.

    • Dorthe Dahl-Jensen
    Nature Geoscience 11, 703–704
  • News and Views |

    The Laurentide Ice Sheet sapped the strength of the North American monsoon during the last ice age, but the ice sheet’s grip on the monsoon weakened as it retreated northwards.

    • Sarah E. Metcalfe
    Nature Geoscience 11, 802–803
  • News and Views |

    There was minimal cooling in the North Atlantic Ocean during the Oligocene inception of the Antarctic ice sheet, according to a sediment record. This finding suggests asynchronous climate changes in the Northern and Southern hemispheres.

    • Timothy Herbert
    Nature Geoscience 11, 624–625