Early Cretaceous abietoid Pinaceae from Mongolia and the history of seed scale shedding
Early Cretaceous abietoid Pinaceae from Mongolia and the history of seed scale shedding
复制标题
蒙古早白垩世松科松科植物及其籽鳞脱落历史
DOI:
10.1002/ajb2.1713
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发表时间:
2021
影响因子:
3
通讯作者:
Herendeen, Patrick S.
中科院分区:
文献类型:
--
作者:
Herrera, Fabiany;Shi, Gongle;Bickner, Maya A.;Ichinnorov, Niiden;Leslie, Andrew B.;Crane, Peter R.;Herendeen, Patrick S.
PremiseSeed cones of extant Pinaceae exhibit two mechanisms of seed release. In “flexers” the cone scales remain attached to the central axis, while flexing and separating from each other to release the seeds. In “shedders” scales are shed from the axis, with the seeds either remaining attached to the scale or becoming detached. The early fossil history of Pinaceae from the Jurassic to Early Cretaceous is dominated by flexing seed cones, while the systematic information provided by shedding fossil cones has been overlooked and rarely integrated with data based on compression and permineralized specimens. We describe the earliest and best‐documented evidence of a “shedder” seed cone from the Aptian–Albian of Mongolia.MethodsLignite samples from Tevshiin Govi locality were disaggregated in water, washed, and dried in air. Fossils were compared to material of extant Pinaceae using LM and CT scans.ResultsLepidocasus mellonaegen. et sp. nov. is characterized by a seed cone that disarticulated at maturity and shed obovate bract–scale complexes that have a distinctive ribbed surface and an abaxial surface covered with abundant trichomes. The ovuliferous scale has ca. 30–40 resin canals, but only scarce xylem near the attachment to the cone axis. Resin vesicles are present in the seed integument. Phylogenetic analysis placesLepidocasusas sister to extantCedruswithin the abietoid grade.ConclusionsThe exquisite preservation of the trichomes inL. mellonaeraises questions about their potential ecological function in the cones of fossil and living Pinaceae.Lepidocasus mellonaealso shows that a shedding dispersal syndrome, a feature that has often been overlooked, evolved early in the history of Pinaceae during the Early Cretaceous.