Suciacarpa is an extinct genus of asterid in the order Cornales. It is known from the fossil species Suciacarpa starrii and Suciacarpa xiangae, both found in Western North America.
At time of description the S. starrii holotype specimen, UF 19276-54286, and paratype, UF 19304-54982, were residing in the paleobotany collections housed by the Florida Museum of Natural History. The two fruits were first studied by Oregon State University paleobotanist Brian Atkinson, with his 2016 type description for the genus and species being published in the NRC Research Press journal Botany. Atkinson coined the genus name Suciacarpa as a combination of "Sucia" after the type locality and the Greek language carpa meaning fruit. The specific epithet starrii was chosen as a patronym honoring David W. Starr, who helped collect the fossils and to increase awareness of Sucia Island in the paleontology community.
The fruits show a mosaic combination of features seen in the Cornales family groups Cornaceae/Alangiaceae and Nyssaceae, Nyssaceae, and Nyssaceae, but does not conform to any one particular family and thus was left as incertae sedis within the order. The Japanese Cornalean species Hironoia described from coalified fossils of Coniacian age differ from Suciacarpa in several ways. The holotype fruit has preserved seeds with fungal hyphae and pyrite crystals in the cell structure.
The only fossil of S. xiangae was found in a calcareous nodule from an outcrop of the late Campanian Spray Formation, part of the Cretaceous Nanaimo Group. The formation outcrop is in the area of Shelter point on the central eastern coast of Vancouver Island, north of Sucuia and Little Sucia Islands.
There is differing opinion regarding what latitude the formations were deposited at in the Campanian. One suggestion, the Baja–British Columbia hypothesis, is that in the Cretaceous the area was located at about 30° north latitude, similar to Modern Baja California, and subsequent tectonic movement has shifted the area north to its present-day location. The other suggestion also involves northward tectonic movement, but suggests the Cretaceous location for the sediments was approximately the region of Northern California.
Description
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