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The Godwin Laboratory for Palaeoclimate Research

 
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A series of 50 minute lectures, followed by discussion, on the broad topic of environmental evolution, climate, ecological and human change during the Quaternary (the last ~2.6 million years). The lectures are aimed at a broad audience (including geoscientists, glaciologists, environmental scientists, atmospheric chemists, biologists, anthropologists and archaeologists). Seminars are on Wednesdays in the Department of Geography Small Lecture Theatre (Downing Site), starting at 17:30. Refreshments are served after the talks and there is time for discussion over drinks and/or dinner. QDG is currently organised by Jinheum Park and Isobel Rowell, supported by David Hodell, Christine Lane, Francesco Muschitiello and Eric Wolff. Please feel free to contact us with queries and suggestions. To sign up to the QDG mailing list, follow this link: https://lists.cam.ac.uk/mailman/listinfo/soc-qdg-quaternary-disc-reminder
Updated: 31 min 44 sec ago

Wed 12 Jun 17:30: Title to be confirmed

Wed, 31/01/2024 - 14:22
Title to be confirmed

Abstract not available

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Wed 21 Feb 17:30: Microplastics from geologists' perspective Building doors are card operated, so latecomers may not be able to access the venue.

Mon, 22/01/2024 - 10:41
Microplastics from geologists' perspective

Abstract not available

Building doors are card operated, so latecomers may not be able to access the venue.

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Wed 07 Feb 17:30: The West Antarctic Ice Sheet and sea level in the last interglacial Building doors are card operated, so latecomers may not be able to access the venue.

Mon, 15/01/2024 - 13:40
The West Antarctic Ice Sheet and sea level in the last interglacial

There is intense interest in the future stability of the West Antarctic Ice Sheet (WAIS). Models range widely in their predictions and in the physics they include. We can constrain possible outcomes by observing what happened to ice sheets at previous times when the polar regions were warmer than present. The last interglacial (LIG) is a particularly important time because both Greenland and Antarctic temperature were higher than present and so was sea level.

Within the WACSWAIN (WArm Climate Stability of the West Antarctic ice sheet in the last INterglacial) project, in 2019 we retrieved a 651 metre ice core to the bed of Skytrain Ice Rise. This ice rise is adjacent to the Ronne Ice Shelf and the WAIS , an therefore sensitive to their extent. The ice core has been processed and analysed continuously for a range of analytes, and we can show that ice from the LIG is present.

I will start by describing the project, fieldwork and analyses. Eventually, I will show what happened to the ice around Skytrain Ice Rise in the LIG , and discuss how this fits with other evidence about LIG sea level.

Building doors are card operated, so latecomers may not be able to access the venue.

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Wed 21 Feb 17:30: TBC Building doors are card operated, so latecomers may not be able to access the venue.

Wed, 10/01/2024 - 12:51
TBC

Abstract not available

Building doors are card operated, so latecomers may not be able to access the venue.

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Wed 07 Feb 17:30: TBC Building doors are card operated, so latecomers may not be able to access the venue.

Wed, 10/01/2024 - 12:49
TBC

Abstract not available

Building doors are card operated, so latecomers may not be able to access the venue.

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