Late Cretaceous climate signal of the Northern Pekulney Range Flora of northeastern Russia

2005 ◽  
Vol 217 (1-2) ◽  
pp. 25-46 ◽  
Author(s):  
Helen J. Craggs
Palaeobotany ◽  
2013 ◽  
Vol 4 ◽  
pp. 148-167 ◽  
Author(s):  
L. B. Golovneva

New investigation of fossil plants from volcanic-sedimentary deposits of the Amka Formation in Ulya River basin (southern part of the Okhotsk-Chukotka volcanogenic belt, Northeastern Russia) shows, that the Arinda, Uenma, Ust-Amka and Gyrbykan floristic assemblages from diff erent localities of this formation have very close systematic composition. We propose to joint these assemblages in the single regional flora, which is named the Ulya flora. The Ulya flora consists of almost 40 species. The majority of them are represented by new undescribed taxa. In this flora gymnosperms (Phoenicopsis ex gr. speciosa Heer, Ginkgo ex gr. adiantoides (Ung.) Heer, G. ex gr. sibirica Heer, Sphenobaiera sp., Podozamites sp., Elatocladus spp., Araucarites sp., Sequoia sp., Metasequoia sp., Cupressinocladus sp., Ditaxocladus sp., Pityophyllum sp., Pityostrobus sp.) predominate. Ferns (Asplenium dicksonianum Heer, Arctopteris sp., Cladophlebis spp. and several undescribed taxa) and angiosperms (Trochodendroides spp., undetermined Platanaceae, Dicotylophyllum spp., Quereuxia angulate (Newb.) Krysht. ex Baik.) are not abundant. This flora is characterized by presence of the Early Cretaceous relicts (Phoenicopsis, Sphenobaiera and Podozamites), by rarity of angiosperms and by high endemism. On the base of comparison of the Ulya flora with other floras from middle and northern parts of the Okhotsk-Chukotka volcanogenic belt, the age of the Ulya flora is estimated as the Coniacian.


Palaeobotany ◽  
2016 ◽  
Vol 7 ◽  
pp. 66-79 ◽  
Author(s):  
D. A. Yudova ◽  
L. B. Golovneva ◽  
P. I. Alekseev

New findings of the genus Dalembia from Late Cretaceous sediments are described: Dalembia sp. from lower part of the Sym Formation (Coniacian – Santonian) of Eastern Siberia; Dalembia sp. from upper part of the Timmerdyakch Formation (Turonian – Coniacian) of Western Siberia; D. vachrameevii E. Lebedev et Herman and the new species D. argentea Yudova et Golovneva from the Chingandzha Formation (Turonian – Coniacian) of Okchotsk-Chukotka volcanogenic belt (Northeastern Russia). The stratigraphic range of the genus Dalembia stretch from the late Albian to Campanian. The geographical area includes the territories of Alaska, northern China, Northeastern Russia, Western and Eastern Siberia. The highest quantity of occurrences associated with Nothern Pacific region.


Palaeobotany ◽  
2015 ◽  
Vol 6 ◽  
pp. 80-95 ◽  
Author(s):  
D. A. Yudova ◽  
L. B. Golovneva

New species Sequoia ochotica Yudova et Golovn. (Pinopsida, Cupressaceae) from the Turonian-Coniacian deposits of the Arman and Chingandzha Formations of the Okhotsk-Chukotka volcanic belt is described based at morphological features of leaves and shoots. Two other Late Cretaceous species of this genus: S. minuta Sveshn. from the Vilyui River basin of Eastern Siberia and S. tenuifolia (Schmalh.) Sveshn. et Budants. from the New Siberian Islands have comparable shoot morphology, but these species were described based at epidermal features.


2016 ◽  
Vol 24 (7) ◽  
pp. 651-760 ◽  
Author(s):  
A. B. Herman ◽  
L. B. Golovneva ◽  
S. V. Shczepetov ◽  
A. A. Grabovsky

Palaeobotany ◽  
2014 ◽  
Vol 5 ◽  
pp. 60-72 ◽  
Author(s):  
D. A. Yudova ◽  
L. B. Golovneva

Three species of Trochodendroides were described fr om the Late Cretaceous deposits of the Chingandzha Formation. Two of them (T. tumanensis Yudova, sp. nov. and T. deminii Yudova et Golovn., sp. nov.) were described as new species, and one was described as Trochodendroides sp. Comparison of new species of the genus Trochodendroides of the Chingandzha flora with representatives of this genus in other Late Cretaceous floras of Northeastern Russia shows that they were presented in composition of the Coniacian Tylpegyrgynai flora of the Pekulnei ridge too, wh ere they were described with other species names (Trochodendroides arctica (Heer) Berry, and Zizyphus smilacifolia Budants.). The presence of the same species shows a similarity of the Chingandzha with Tylpegyrgynai flora and confirms the Coniacian age of the Chingandzha flora.


Sign in / Sign up

Export Citation Format

Share Document