{"refrec":{"BRefID":410386,"RR":"<b>Gale, A.S.</b> (2025). British Fossil Cirripedia. Part 2, Calanticomorpha, Scalpellomorpha. <i>Monograph of the Palaeontographical Society 179(671)</i>: 105-193. <a href=\"https://dx.doi.org/10.1080/02693445.2025.2494375\" target=\"_blank\">https://dx.doi.org/10.1080/02693445.2025.2494375</a>","BEntID":408195,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Monograph of the Palaeontographical Society 179(671)</i>: 105-193. <a href=\"https://dx.doi.org/10.1080/02693445.2025.2494375\" target=\"_blank\">https://dx.doi.org/10.1080/02693445.2025.2494375</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Gale, A.S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Gale, A.S.","Englishabstract":"Cretaceous and Cenozoic pedunculate cirripedes of the Orders Calanticomorpha and Scalpellomorpha are described and illustrated. These include a total of 29 genera, of which four are new (<i>Bognorscalpellum, Solidoscalpellum, Lacrymascalpellum, Laeviscalpellum</i>) and 76 species, of which 14 are new. Of the fauna, eight come from the Lower Cretaceous (Weald, Lower Greensand and Selborn groups), 46 from the Upper Cretaceous (Chalk Group), 20 from the Paleogene (Thames, Bracklesham, Barton and Solent groups) and two from the Neogene (Crag Group). The study demonstrates the extraordinary diversity of Upper Cretaceous pedunculate cirripedes, of which many went extinct at the K-Pg boundary, although some survived to the present day in the deep sea.","AbstractOtherLang":"Les cirripèdes pédonculés crétacés et cénozoïques des ordres Calanticomorpha et Scalpellomorpha sont décrits et illustrés. Ils comprennent un total de 29 genres, dont quatre sont nouveaux (<i>Bognorscalpellum, Solidoscalpellum, Lacrymascalpellum, Laeviscalpellum</i>) et 76 espèces, dont 14 sont nouvelles. Parmi ces espèces, huit proviennent du Crétacé inférieur (groupes Weald, Lower Greensand et Selborne), 46 du Crétacé supérieur (groupe Craie), 20 de l’Éocène et de l’Oligocène (groupes Thames, Bracklesham, Barton et Solent) et deux du Pliocène (groupe Crag). L’étude démontre l’extraordinaire diversité des cirripèdes pédonculés du Crétacé supérieur, dont beaucoup se sont éteints à la limite Crétacé/Paléogène, bien que certains aient survécu jusqu’à aujourd’hui dans les grands fonds.","BibLvlCode":"AS","StandardTitle":"British Fossil Cirripedia. 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