Liquidambar changii

Life-forms

Classification System: APG IV

Superregnum: Eukaryota
Regnum: Plantae
Cladus: Angiosperms
Cladus: Eudicots
Cladus: Core eudicots
Ordo: Saxifragales

Familia: Altingiaceae
Genus: Liquidambar
Species: †L. changii
Name

Liquidambar changii Pigg, Ickert-Bond, Wen 2004
Type locality

Middle Miocene, Museum Flow Package, Sentinel Bluffs Unit, Central Columbia Plateau N2 Grande Ronde Basalt, Columbia River Basalt Group; "Hi Hole", ~7.3 km north of the Interstate 82 Firing Center Exit, Yakima County, Washington, USA.
Type material

Holotype: Burke Museum of Natural History and Culture, University of Washington, Seattle, Washington, USA UWBM 45-I
Paratypes: Burke Museum of Natural History and Culture, University of Washington, Seattle, Washington, USA UWBM 97418, UWBM 97419, UWBM 97420, UWBM 55136, UWBM 55145, UWBM 55143, UWBM 97421, UWBM 55111, UWBM 97422, UWBM 94724, UWBM 55104, UWBM 55131 #9 bot, UWBM 97425, UWBM 55133, UWBM 55078, UWBM 55084, UWBM 55104, UWBM 55107, UWBM 55111, UWBM 55129, UWBM 55131, UWBM 55136, UWBM 97417–97441, UWBM 97417, UWBM 97426–97441
Paratypes: Arizona State University, Tempe, AZ, USA ASU-YC-np8, ASU-YC-np26, ASU-YCT6–9, ASU-YC13.ASU-YCT 11, ASU-YC 97, ASU-2 top.

References

Pigg, Kathleen B., Ickert-Bond, Stefanie M., & Wen, Jun (2004); "Anatomically preserved Liquidambar (Altingiaceae) from the middle Miocene of Yakima Canyon, Washington state, USA, and its biogeographic implications" American Journal of Botany 91(3):499-509

Liquidambar changii is an extinct species of sweetgum in the Altingiaceae genus Liquidambar. Liquidambar changii is known from Middle Miocene fossils found in Central Washington.
History and classification

The species was first described from specimens of silicified infructescences in blocks of chert. The chert was recovered from the "Hi hole" site, one of the "county line hole" fossil localities north of Interstate 82 in Yakima County, Washington.[1] The "Hi hole" site works strata which was thought to be part of the Museum Flow Package within the interbeds of the Sentinel Bluffs Unit of the central Columbia Plateau N2 Grande Ronde Basalt, Columbia River Basalt Group. The Museum Flow Package interbeds, designated the type locality, are dated to the middle Miocene and are approximately 15.6 million years old.[2] Later re-evaluation of the "hi hole" site indicated that the site is included into a basalt flow, rather than part of the interbedded Museum flow package. The evaluation suggested the basalt is part of the Wanapum Basalt and that the fossils are possibly a little younger than formerly reported.[1] Dating reported in 2007 of a related site near Ellensburg, Washington confirmed that the deposits worked are pockets within the basalt flows, and the 15.6 million year old date was accurate.[3]

At the time of study, the holotype infructescence, specimen UWBM 94723, and a series of paratype specimens are preserved in chert blocks housed in the Burke Museum of Natural History and Culture while an additional seven of the paratypes were part of the paleobotanical collections at Arizona State University. The specimens represent a range of preservation conditions, ranging from exposed on weathered surfaces of the chert, totally weathered out of the chert, and as hollow chert casts of the infructescences. A total of 42 specimens in chert were studied by paleobotanists Kathleen Pigg, Stefanie Ickert-Bond, and Jun Wen, with their 2004 type description being published in the American Journal of Botany. Pigg and team chose the specific epithet changii as a patronym honoring the Chinese botanist and ecologist Hung-ta Chang, for his work with the family Altingiaceae and for describing the living species Liquidambar acalycina.[1]

Based on the infructescence morphology, Pigg et al noted the close similarity between L. changii and L. acalycina, suggesting they are possibly closely related. Due to the lack of some details used for the delimitation of L. acalycina, they chose to place the fossils into a new species rather than describe them as fossils belonging to the living species. The authors also noted that a number of Liquidambar compression/impression fossils of very similar age have been reported from the region, and may be also closely related, but lack the needed detail for examination.[1]
Description

Liquidambar changii infructescences are round in shape, with diameters reaching 2.5 cm (0.98 in), consisting of as many as 30 individual capsules in a helical arrangement. The infructescences are born on woody stems of up to 16 mm (0.63 in) and several specimens have stems containing secondary xylem. The woody structuring of the stems occasionally extends into the infructescence and all of the specimens have ducts for resin or gum, a character seen in living Liquidambar. The individual capsules are bi-locular with elongated outlines that are open at the top, and closed at the base which attaches to the central axis of the fruit. In each capsule there are between 5 and 9 aborted seeds and between one and two mature seeds, attached to the interior of the capsule along the side that is fused to the adjoining capsule. The mature seeds are attached to the capsule near the fruit interior while the aborted seeds are found both near the interior and to the sides of the ventral margin. The mature fruits have a triangular outline and have a raised ridge that runs around the outside of the seed.[1]
References

Pigg, K. B.; Ickert-Bond, S. M.; Wen, J. (2004). "Anatomically preserved Liquidambar (Altingiaceae) from the middle Miocene of Yakima Canyon, Washington state, USA, and its biogeographic implications". American Journal of Botany. 91 (3): 499–509. doi:10.3732/ajb.91.3.499. PMID 21653405.
Pigg, K.B. (2001). "Anatomically preserved Woodwardia virginica (Blechnaceae) and a new Filicalean fern from the Middle Miocene Yakima Canyon Flora of central Washington, USA". American Journal of Botany. 88 (5): 777–787. doi:10.2307/2657030. JSTOR 2657030.
Pigg, K. B.; DeVore, M. D.; Benedict, J. C.; Creekmore, R. M. (2014). "Fruits of Melia (Meliaceae, Melioideae) from the Middle Miocene Yakima Canyon Flora of Central Washington State, USA". Paleobotany and Biogeography: A Festschrift for Alan Graham in His 80th Year: 326–337.