
Benjamin Mills
@bjwmills
ID: 943201598158901248
19-12-2017 19:29:19
433 Tweet
726 Followers
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Article: Enhanced chemical weathering following continental breakup may have driven a succession of Mesozoic oceanic anoxic events, according to tectonic and biogeochemical modelling Prof Tom Gernon Benjamin Mills OceanEarthUniSoton University of Southampton Earth and Environment at Leeds nature.com/articles/s4156…


We have a 3-yr position in the group to work on European climate projections and implications for food safety as part of the European Commission project Ambrosia. Climate scientists with an interest in climate impacts please apply! Closes 27 Sept. @ICASLeeds jobs.leeds.ac.uk/vacancy.aspx?r…

Enhanced chemical weathering following continental breakup may have driven a succession of Mesozoic oceanic anoxic events, according to tectonic and biogeochemical modelling presented in Nature Geoscience. go.nature.com/4cVXQdf


#WeekendReading: Gernon et al. (Prof Tom Gernon w/Benjamin Mills and others) show that enhanced weathering of mafic rocks during continental breakup and early seafloor spreading could drive a succession of #anoxic events. (remember - weathering releases nutrients) nature.com/articles/s4156…

Fully-funded 4 year PhD to study CO2 release from sedimentary rocks during past warm climates. Work with me, Richard Stockey, Prof Tom Gernon + Benjamin Mills. Due to funding restrictions, UK-based students only. Deadline 17.10.24. Start date flexible. Please RT. tinyurl.com/5xfbb9de

Come and and do a fully-funded PhD with us at OceanEarthUniSoton! Please share widely and feel free to get in touch with any questions about this really exciting project. southampton.ac.uk/study/postgrad…










📢 PLEASE RT! ☁️ M2 Masters Internship in Atmosphere Habitability Modelling 🎓 6-month paid opportunity starting early 2025 🦠 Investigate habitability & microbial ecology of the atmosphere 💻 Theoretical & numerical modelling ☀️ Marseille, France 👨🔬 James Bradley @soundslikealloy



Article: Cryptic degassing, whereby mantle-derived CO2 fluxes continue after surface eruptions slow, can explain prolonged warming that followed some large igneous province events Ben Black Benjamin Mills Tamsin Mather Volcano Listening Project C2C nature.com/articles/s4156…


The first of hopefully many papers from our U.S. National Science Foundation funded @c2c_proj, suggesting that cryptic degassing driven by a rheologic phase transition in the crust (shutting off LIP eruptions) drives prolonged warming periods in Earth History. Ben Black Tamsin Mather Benjamin Mills and others.