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Items where Author is "Hoyal Cuthill, Jennifer F"

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Number of items: 7.

Article

Hoyal Cuthill, Jennifer F and Hunter, Aaron W (2020) Fullerene‚Äźlike structures of Cretaceous crinoids reveal topologically limited skeletal possibilities. Palaeontology, 63 (3). pp. 513-524. DOI https://doi.org/10.1111/pala.12474

Han, Jian and Conway Morris, Simon and Hoyal Cuthill, Jennifer F and Shu, Degan (2019) Sclerite-bearing annelids from the lower Cambrian of South China. Scientific Reports, 9 (1). 4955-. DOI https://doi.org/10.1038/s41598-019-40841-x

Hoyal Cuthill, Jennifer F and Guttenberg, Nicholas and Ledger, Sophie and Crowther, Robyn and Huertas, Blanca (2019) Deep learning on butterfly phenotypes tests evolution’s oldest mathematical model. Science Advances, 5 (8). eaaw4967-. DOI https://doi.org/10.1126/sciadv.aaw4967

Hoyal Cuthill, Jennifer F and Han, Jian (2018) Cambrian petalonamid Stromatoveris phylogenetically links Ediacaran biota to later animals. Palaeontology, 61 (6). pp. 813-823. DOI https://doi.org/10.1111/pala.12393

Hoyal Cuthill, Jennifer F and Conway Morris, Simon (2017) Nutrient-dependent growth underpinned the Ediacaran transition to large body size. Nature Ecology and Evolution, 1 (8). pp. 1201-1204. DOI https://doi.org/10.1038/s41559-017-0222-7

Hoyal Cuthill, Jennifer F and Sewell, Kim B and Cannon, Lester RG and Charleston, Michael A and Lawler, Susan and Littlewood, D Timothy J and Olson, Peter D and Blair, David (2016) Australian spiny mountain crayfish and their temnocephalan ectosymbionts: an ancient association on the edge of coextinction? Proceedings of the Royal Society B: Biological Sciences, 283 (1831). p. 20160585. DOI https://doi.org/10.1098/rspb.2016.0585

Hoyal Cuthill, Jennifer F and Conway Morris, Simon (2014) Fractal branching organizations of Ediacaran rangeomorph fronds reveal a lost Proterozoic body plan. Proceedings of the National Academy of Sciences, 111 (36). pp. 13122-13126. DOI https://doi.org/10.1073/pnas.1408542111

This list was generated on Thu Feb 2 12:08:07 2023 GMT.