Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic
Mesoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Galenki Formation
Click to display on map of the Ancient World at:
Galenki Fm base reconstruction

Galenki Fm


Period: 
Cretaceous

Age Interval: 
mid Cretaceous (S-10)


Province: 
Siberia southeast

Type Locality and Naming

Razdolny depression of southern Primorye Basin (S-10; NW of Vladivostok). Upper formation of Nikan Gr.


Lithology and Thickness

It is composed of tuffaceous sandstones with interbeds of siltstones, mudstones and coal with a total thickness of up to 500m (Turbin, 1994).


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

Conformable onto Lipovtsy Fm of Nikan Gr

Upper contact

Conformably overlain by Korkino Gr

Regional extent


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[131.2,42.7],[132.2,43.2],[132.5,43.6],[132,44.2],[132,44.6],[131.3,44.3],[131.2,42.7]]]]}}

Fossils

Three flora assemblages were identified in the formation (Volynets, 2005). The Early Galenki assemblage was identified in the lower part of the formation (Volynets, 2006). It is characterized by low taxonomic diversity (31 taxa) with domination of cycadophytes and ferns. The most abundant species are Dictyozamites cordatus, Leptopterophyllum pterophylloides, Nilssonia densinervis, N. ex gr. orientalis, Onychiopsis psilotoides, Teilhardia tenella, Anemia dicksoniana, Ginkgo ex gr. adiantoides, Lycopodites prynadae, Podozamites tenuinervis, Sagenopteris aff. mantellii. The defining feature of this flora assemblage is the domination of Early Cretaceous cycadophytes and the increase of representatives of “young” genera of ferns. The Middle Galenki assemblage was identified in the middle part of the Galenki Formation. It is characterized by high taxonomic diversity (69 taxa) with domination of ferns (27 taxa). The typical taxa of the assemblage are represented by Birisia alata, Anemia dicksoniana, Lobifolia novopokrovskii, Podozamites tenuinervis, Taxites brevifolius, Sequoia reichenbachii, Neozamites denticulatus, Pterophyllum sutschanense, Nilssonia canadensis, N. ex gr. orientalis, Sapindopsis, Dicotylophyllum, Cercidiphyllum. The feature of this assemblage is the domination of ferns (39%) and conifers (20%) with a significant presence of Birisia, Anemia, Dicksonia, Adiantopteris, Taxites, Sequoia and the appearance of angiosperms. The Late Galenki flora assemblage was identified in the upper part of the Galenki Formation in the Razdolnaya and Amba rivers basin, on the Muraviev-Amurskiy Peninsula and in the Khanka lake region (Volynets, 2015; Volynets and Bugdaeva, 2017). It is characterized by high taxonomic diversity (86 taxa) with domination of ferns (27 taxa) and cycadophytes (25 taxa). The typical taxa of the assemblage are represented by ferns Osmunda denticulata, Anemia dicksoniana, Gleichenites porsildii, Birisia oerstedtii, Cyathea aff. tyrmensis, Eogymnocarpium sinense, Lobifolia novopokrovskii, cycadophytes Pterophyllum burejense, P. sutschanense, Leptopterophyllum pterophylloides, Encephalartopsis vachrameevii, Nilssonia canadensis, N. ex gr. brongniartii, conifers Podozamites tenuinervis, Sequoia reichenbachii, Taxites acuminatus, T. brevifolius and Athrotaxopsis expansa.


Age 


Age Span: 

    Beginning stage: 
Albian

    Fraction up in beginning stage: 
0.15

    Beginning date (Ma): 
111.30

    Ending stage: 
Albian

    Fraction up in the ending stage: 
0.85

    Ending date (Ma):  
102.41

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Igor N. Kosenko, Jingeng Sha and Boris N. Shurygin (2021). Upper Mesozoic stratigraphy of Sikhote-Alin (Russian Far East) and northeastern China: Non-marine and marine correlations. Part 1: Upper Jurassic-Hauterivian AND 2. Barremian-Aptian. Cretaceous Research, 124: articles 104811 (https://doi.org/10.1016/j.cretres.2021.104811) AND 104812 (https://doi.org/10.1016/j.cretres.2021.104812)