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<mods:title id="B5C2482A5EA643FC1A7E89FC8DC74FAC">Phylogeny of the deep-sea cirripede family Scalpellidae (Crustacea, Thoracica) based on shell capitular plate morphology</mods:title>
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FAMILY
<taxonomicName id="4C7FFFC0CC0F0D4751D0FE12BA0F64EB" ID-CoL="FZK" ID-ENA="37543" authority="PILSBRY, 1907" authorityName="PILSBRY" authorityYear="1907" box="[1013,1348,459,480]" class="Maxillopoda" family="Scalpellidae" kingdom="Animalia" order="Pedunculata" pageId="30" pageNumber="296" phylum="Arthropoda" rank="family">
SCALPELLIDAE
<bibRefCitation id="EFEEF9B2CC0F0D475687FE12BA0F64EB" author="Pilsbry HA" box="[1186,1348,459,480]" pageId="30" pageNumber="296" pagination="1 - 122" refId="ref23802" refString="Pilsbry HA. 1907. The barnacles (Cirripedia) contained in the collections of the U. S. National Museum. Bulletin of the United States National Museum 60: 1 - 122, 11 pls." type="book chapter" year="1907">PILSBRY, 1907</bibRefCitation>
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<emphasis id="B90B5851CC0F0D475119FE28BB5F670D" box="[828,1044,497,518]" italics="true" pageId="30" pageNumber="296">Modified diagnosis</emphasis>
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<paragraph id="8BC08443CC0F0D475119FDC9BA77678A" blockId="30.[828,1443,497,641]" pageId="30" pageNumber="296">Scalpellomorphs that possess a maximum of 14 plates (carina, rostrum, paired scuta, terga, upper latera, carinolatera, rostrolatera, and inferior median latera), rarely 13, by secondary loss of the rostrum.</paragraph>
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<emphasis id="B90B5851CC0F0D475119FD75BCEA67CA" box="[828,929,684,705]" italics="true" pageId="30" pageNumber="296">Remarks</emphasis>
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This definition works effectively for all known living and fossil forms, with the exception of the highly derived
<taxonomicName id="4C7FFFC0CC0F0D475119FCD1BBB46616" authority="Broch, 1922" authorityName="Broch" authorityYear="1922" box="[828,1279,776,798]" class="Maxillopoda" family="Scalpellidae" genus="Scalpellopsis" higherTaxonomySource="GBIF" kingdom="Animalia" order="Pedunculata" pageId="30" pageNumber="296" phylum="Arthropoda" rank="species" species="striatociliata">
<emphasis id="B90B5851CC0F0D475119FCD1BB216616" box="[828,1130,776,797]" italics="true" pageId="30" pageNumber="296">Scalpellopsis striatociliata</emphasis>
<bibRefCitation id="EFEEF9B2CC0F0D475656FCD1BBB46616" author="Broch H" box="[1139,1279,776,798]" pageId="30" pageNumber="296" pagination="215 - 358" refId="ref22211" refString="Broch H. 1922. Papers from Dr. Th. Mortensen's Pacific Expedition. 1914 - 16. No. X. Studies on Pacific Cirripeds. Videnskabelige Meddelelser fra Dansk Naturhistorisk Forening 73: 215 - 358." type="journal article" year="1922">Broch, 1922</bibRefCitation>
</taxonomicName>
. The record of a subcarina in the Cretaceous species
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<emphasis id="B90B5851CC0F0D4756C8FCFFBCC06651" italics="true" pageId="30" pageNumber="296">Diotascalpellum fossula</emphasis>
(
<bibRefCitation id="EFEEF9B2CC0F0D4751BFFC9CBB096650" author="Darwin CR" box="[922,1090,837,859]" pageId="30" pageNumber="296" refId="ref22650" refString="Darwin CR, 1851 b. A monograph on the Fossil Lepadidae, or pedunculated cirripedes of Great Britain. Palaeontographical Society (Monograph), 88." type="book" year="1851">Darwin, 1851b</bibRefCitation>
)
</taxonomicName>
by
<bibRefCitation id="EFEEF9B2CC0F0D475651FC9CBA5B6650" author="Hebert E" box="[1140,1296,837,859]" pageId="30" pageNumber="296" pagination="345 - 374" refId="ref23167" refString="Hebert E. 1855. Tableau des fossiles de la Craie de Meudon, et description de quelques especes nouvelles. Memoires de la Societe geologique de France 5: 345 - 374." type="journal article" year="1855">Hébert (1855)</bibRefCitation>
and
<bibRefCitation id="EFEEF9B2CC0F0D47576FFC9CBCC86672" author="Withers TH" pageId="30" pageNumber="296" refId="ref24298" refString="Withers TH. 1935. British Museum (Natural History). Catalogue of fossil Cirripedia in the Department of Geology. Vol. II, Cretaceous. xvi + 534 pp., 50 pls. London: Trustees of the British Museum (Natural History)." type="book" year="1935">Withers (1935)</bibRefCitation>
is not substantiated by a re-examination of the material. The family appears in the Aptian (Early Cretaceous, about 120 Mya), and is represented by abundant fossil and living forms. In the Cretaceous and the Palaeogene, species were common in shallow and deep marine environments, with palaeodepths of as little as
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20
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. Neogene and present-day records are almost exclusively from the deep sea. The present study identifies two groups, which are taken as subfamilies.
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