Publications
2017
Terreneuvian Stratigraphy and Faunas from the Anabar Uplift, Siberia. Acta Palaeontologica Polonica 62, 311-440. doi:10.4202/app.00289.2016
, 2017. The agnostoid arthropod Lotagnostus Whitehouse, 1936 (late Cambrian; Furongian) from Avalonian Cape Breton Island (Nova Scotia, Canada) and its significance for international correlationAbstract. Geological Magazine 154, 1001-1021. doi:10.1017/S0016756816000571
, 2017. Integrated stratigraphic, geochemical, and paleontological late Ediacaran to early Cambrian records from southwestern Mongolia: Comment. Geological Society of America Bulletin 129, 1012-1015. doi:10.1130/B31640.1
, 2017. 2016
The Precambrian–Phanerozoic and Ediacaran–Cambrian Boundaries: A Historical Approach to a Dilemma, in: , Earth System Evolution And Early Life: A Celebration Of The Work Of Martin Brasier. Geological Society of London, London, England, pp. 311-349. doi:10.1144/SP448.10
, 2016. Rapid changes of magnetic Field polarity in the late Ediacaran: Linking the Cambrian evolutionary radiation and increased UV-B radiation. Gondwana Research 34, 149–157. doi:10.1016/j.gr.2016.01.001
, 2016. Dodging snowballs: Geochronology of the Gaskiers glaciation and the first appearance of the Ediacaran biota. Geology 44, 955-958. doi:10.1130/G38284.1
, 2016. Geological context, biostratigraphy and systematic revision of late early Cambrian olenelloid trilobites from the Parker and Monkton formations, northwestern Vermont, U.S.A.. Australasian Palaeontological Memoirs 49, 193-240.
, 2016. Comment on “Terreneuvian Small Shelly Faunas of East Yunnan (South China) and Their Biostratigraphic Implications”. Palaeogeography, Palaeoclimatology, Palaeoecology doi: 10.1016/j.palaeo.2016.04.016. doi:10.1016/j.palaeo.2016.04.016
, 2016. Correlation of the Cambrian Evolutionary Radiation: geochronology, evolutionary stasis of earliest Cambrian (Terreneuvian) small shelly fossil (SSF) taxa, and chronostratigraphic significance. Geological Magazine 153, 750-756. doi:10.1017/S0016756815001089
, 2016. 2015
Late Cambrian (middle Furongian) Shallow-Marine Dysoxic Mudstone with Calcrete and Brachiopod–Olenid–Lotagnostus Faunas in Avalonian Cape Breton Island, Nova Scotia. Geological Magazine 152, 973-992. doi:10.1017/S001675681400079X
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