2015
DOI: 10.1016/j.cretres.2014.12.014
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A Taxus leafy branch with attached ovules from the Lower Cretaceous of Inner Mongolia, North China

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Cited by 17 publications
(6 citation statements)
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“…The most recent common ancestor of Cephalotaxaceae and Taxaceae was set to a minimum age of 163.5 Mya ( Florin, 1963 ). The stem age of Taxus was set to a minimum age of 100 Mya ( Xu et al , 2015 ). We used the uncorrelated log-normal relaxed molecular clock approach, which allows uncertainty in the age of calibrations to be represented as prior distributions rather than as strict calibration/fixed points.…”
Section: Methodsmentioning
confidence: 99%
“…The most recent common ancestor of Cephalotaxaceae and Taxaceae was set to a minimum age of 163.5 Mya ( Florin, 1963 ). The stem age of Taxus was set to a minimum age of 100 Mya ( Xu et al , 2015 ). We used the uncorrelated log-normal relaxed molecular clock approach, which allows uncertainty in the age of calibrations to be represented as prior distributions rather than as strict calibration/fixed points.…”
Section: Methodsmentioning
confidence: 99%
“…A starting tree with branch lengths satisfying all fossil prior constraints was created manually according to the RaxML inferred tree. The node uniting Taxaceae and Cupressaceae was calibrated with a minimum age of 197 Ma (Florin, , ); the age of Taxus was set to a minimum age of 100 Ma (Xu et al, ). We modeled all calibrations as an exponential distribution (Ho & Philips, ) with a mean of 1 and an offset (hard bound constraint) that equaled the minimum age of the calibration.…”
Section: Methodsmentioning
confidence: 99%
“…According to the abovementioned palynological analysis, we name the palynological assemblages of this study area Psophosphaera-Perinopollenites-Cycadopites. (Jin, Wang, & Du, 2013;Xu et al, 2015). Other paleontologists also found a large number of macrofossils in the Guyang Formation (Table 1).…”
Section: Resultsmentioning
confidence: 90%
“…The palynomorph assemblages of the Guyang Basin are dominated by gymnosperm pollen and filicopsida spores. Most of the gymnosperm pollen are conifers pollen represented by Perinopollenites , Classopollis , Piceaepollenites , Taxodites and Araucariacites , contain a large amount of Ginkgoales and Cycad pollen grains, plant macrofossils discovered in the study area, and include Coniopteris simplex , Podozamites lanceolatus , Sequoia gracilis , Ginkgo lepida , Sabinites gracilis , Elatides manchurensis , Elatides sp., Sabinites neimngonglica , Torreya grandis , Stenorachis lepida , Equisetites sp., and Taxus guyangensis (Jin, Wang, & Du, ; Xu et al, ). Other paleontologists also found a large number of macrofossils in the Guyang Formation (Table ).…”
Section: Discussionmentioning
confidence: 99%
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