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Briony Horgan

As seen in: Nature, Wiley Online Library, How Stuff Works, The Conversation, The Daily Beast, Live Science, Phys.org, SPACE.com, Science Magazine, Deccan Herald and
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In Science Journals

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By Ljubica Mihaljevic, Connor C Fausto, Mark S. Aldenderfer, Jelena Stajic Verified, Phil Szuromi, Leslie K. Ferrarelli Verified, Briony Horgan, Unnati Sonawala, Madeleine Seale, L. Bryan Ray Verified, Yevgeniya Nusinovich Verified, Jesse R. Smith, Michael Funk Verified, Di Jiang, Sarah Ross, Priscilla Kelly Verified, YURY SULEYMANOV, Bianca Lopez, Leoma Bere, Courtney S. Malo
| Science Magazine Verified
Archaeology Paleoindian diet in the Western Hemisphere Superconductivity Splitting vortices Ferroelectrics Stepwise switching in dipole layers Magnetism Circumventing spin Quantum Dynamics Localization without disorder Biochemistry Decoding FFAR2 function and pharmacology Planetary Science Organics in an ancient lake on Mars Plant Immunity Splicing flips the immune switch Synthetic Biology Specifying kidney structure in vitro Endocrinology Mapping cell and hormone networks Ice Sheets Rising...
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Igneous and sedimentary origins of Jezero crater units from X-ray crystal mapping on Mars - Communications Earth & Environment

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By Brendan J. Orenstein, David Flannery, Michael Jones, Eleanor Moreland, Kirsten L. Siebach, Michael M. Tice, Allan Treiman, Briony Horgan, Balz Kamber, Athanasios Klidaras, Luke Nothdurft, Yang Liu Verified, Edward A. Cloutis, Abigail C. Allwood, Scott VanBommel
| Nature Verified
Abstract Jezero crater is located in Mars’ largest olivine-rich region, which is variously interpreted as lava flows, intrusive plutons, clastic sediments, or pyroclastics.
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Carbonated ultramafic igneous rocks in Jezero crater, Mars

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By Kenneth H. Williford, Kenneth A. Farley, Briony Horgan, Brad Garczynski
| Science Magazine Verified
Abstract The Perseverance rover landed in Jezero crater on Mars, which once contained a lake of liquid water. We report the rock properties encountered by Perseverance during a ten-kilometer traverse extending over 400 meters in elevation, from beneath Jezero's western sedimentary fan to the upper crater rim. These rocks consist of coarse-grained olivine, magnesium- and iron-carbonates, silica, and phyllosilicates, including some of the oldest materials exposed within Jezero.
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