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Environmental and trilobite diversity changes during the middle-late Cambrian SPICE event
Gill grooming in middle Cambrian and Late Ordovician trilobites
A Glyptagnostus reticulatus trilobite faunule from the Cambrian of the Northern Qilian Mountains, northwest China, and its paleogeographical implications
Cambrian and earliest Ordovician fauna and geology of the Sông Đà and adjacent terranes in Việt Nam (Vietnam)
Absolute axial growth and trunk segmentation in the early Cambrian trilobite Oryctocarella duyunensis
Development of the early Cambrian oryctocephalid trilobite Oryctocarella duyunensis from western Hunan, China
Articulated trilobite ontogeny: suggestions for a methodological standard
Satunarcus , a new late Cambrian trilobite genus from southernmost Thailand and a reevaluation of the subfamily Mansuyiinae Hupé, 1955
Cambrian geology of the Salt Range of Pakistan: Linking the Himalayan margin to the Indian craton: Reply
Cambrian geology of the Salt Range of Pakistan: Linking the Himalayan margin to the Indian craton
Ontogeny of the articulated yiliangellinine trilobite Zhangshania typica from the lower Cambrian (Series 2, Stage 3) of southern China
Cambrian–Ordovician orogenesis in Himalayan equatorial Gondwana
Axial growth gradients across the postprotaspid ontogeny of the Silurian trilobite Aulacopleura koninckii
Cambrian microfossils from the Tethyan Himalaya
Size, shape, and systematics of the Silurian trilobite Aulacopleura koninckii
Plate tectonic influences on Neoproterozoic–early Paleozoic climate and animal evolution
Onset of Maturity and Ontogenetic Tagmatization of the Pygidium in the Development of Lonchopygella megaspina (Trilobita, Later Furongian, Cambrian)
Global Cambrian trilobite palaeobiogeography assessed using parsimony analysis of endemicity
Abstract Palaeobiogeographical data on Cambrian trilobites obtained during the twentieth century are combined in this paper to evaluate palaeoceanographic links through c. 30 myr, once these arthropods biomineralized. Worldwide major tectonostratigraphic units are characterized at series intervals of Cambrian time and datasets of trilobite genera (629 for Cambrian Series 2, 965 for Cambrian Series 3, and 866 for the Furongian Series) are analysed using parsimony analysis of endemicity. Special attention is given to the biogeographical observations made in microcontinents and exotic terranes. The same is done for platform-basinal transects of well-known continental margins. The parsimony analysis of endemicity analysis resulted in distinct palaeogeographical area groupings among the tectonostratigraphic units. With these groupings, several palaeobiogeographical units are distinguished, which do not necessarily fit the previously proposed biogeographical realms and provinces. Their development and spatial distributions are broadly controlled by Cambrian palaeoclimates, palaeogeographical conditions (e.g. carbonate productivity and anoxic conditions) and ocean current circulation. Supplementary material: Global dataset of Cambrian Epoch 2 (A), Cambrian Epoch 3 (B) and the Furongian Epoch (C) trilobite genera are provided at: http://www.geolsoc.org.uk/SUP18669