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   » » Wiki: Suciacarpa
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Suciacarpa is an of in the order . It is known from the fossil species Suciacarpa starrii and Suciacarpa xiangae, both found in Western North America.


History and classification
Suciacarpa is known from several anatomically preserved fruits found in north-western Washington state, United States, and , British Columbia.

At time of description the S. starrii specimen, UF 19276-54286, and , UF 19304-54982, were residing in the 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 carpa meaning fruit. The specific epithet starrii was chosen as a 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 / and , , and , but does not conform to any one particular family and thus was left as within the order. The Japanese Cornalean species described from coalified fossils of age differ from Suciacarpa in several ways. The holotype fruit has preserved seeds with and crystals in the cell structure.


Distribution and paleoecology
The S. starrii holotype specimen was collected on while the paratype was collected on . Both fruits are preserved in recovered from exposures of the age Cedar District Formation. The nodules formed in what is thought to have been a shallow marine shelf environment that also had and . The formation has also preserved fossils of other terrestrial organisms including a single , and a femur, the first dinosaur identified from Washington State.

The only fossil of S. xiangae was found in a calcareous nodule from an of the late Campanian , part of the Cretaceous . 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 , 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
The S. starrii fruits have a four-chambered structure with a smooth, woody exterior endocarp that is formed from tissues. The fruits are approximately in diameter and long with each of the four crescent-shaped chambers opening near the top of the fruit. The germination chambers have a single seed each, attached to the chamber wall near the apex. Based on the positioning of the preserved fungal hyphae, the cells of the seed were rectangular in outline and small. Like members of Nyssaceae, S. starrii has short germination valves that occupy only about half of the fruit, but have secretory chambers, a feature only seen in cornelian cherries of the subgenus Cornus. Also S. starrii has a pair of vascular bundles running through each of the septa lengthwise. The two bundles converge near the top of the septum to enter the seed.

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