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      <image:title>News - Destabilisation of the terrestrial biosphere during past warm climates - Make it stand out</image:title>
      <image:caption>A mock satellite image showing an ice-free and green Antarctic continent ~50 million years ago (Image credit: Dr Alan Kennedy). https://www.science.org/doi/10.1126/science.aad6284</image:caption>
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      <image:caption>Fig. 1. Paleoclimate context for future climate scenarios (Tierney et al., 2020; Science)</image:caption>
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      <image:caption>New article in 'Organic Geochemistry' which discusses the impact of organic carbon reworking on GDGT proxies. To learn more, click here.</image:caption>
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      <image:title>Temperature</image:title>
      <image:caption>Fig.1. IsoGDGTs typically found in marine sediments.</image:caption>
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      <image:title>Temperature</image:title>
      <image:caption>Fig. 2. Typical distribution of isoGDGTs in “cold” and “warm” settings.</image:caption>
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      <image:title>Temperature</image:title>
      <image:caption>Fig.3. 5-methylated brGDGTs typically found in terrestrial sediments.</image:caption>
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      <image:caption>Figure 1. Schematic representation of how the wetland methane cycle operates. Methane can be released to atmosphere via plants, bubbles or diffusion. However, it can also be consumed by methanotrophic bacteria (Credit: G. Inglis)</image:caption>
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