Podozamites is an extinct genus of fossil conifer leaves. In its broader sense, it has been used as a morphogenus (form taxon) to refer to any broad leaved multi-veined conifer leaves. Modern broad-leaved conifers with a similar form include Agathis in the family Araucariaceae and Nageia in Podocarpaceae, with some Podozamites sensu lato probably belonging to the same families.[1]
| Podozamites Temporal range:
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|---|---|
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| Fossil Podozamites from China | |
Scientific classification 
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| Kingdom: | Plantae |
| Clade: | Tracheophytes |
| Clade: | Gymnospermae |
| Division: | Pinophyta |
| Class: | Pinopsida |
| Genus: | †Podozamites Braun 1843 |
In a more narrow sense, Podozamites has been used to refer to the leaves of a probably monophyletic group of deciduous broad leafed voltzialean conifers which lived in the Northern Hemisphere, particularly East Asia and Siberia, during the Late Triassic to early Late Cretaceous, where it formed part of wet coal swamp communities.[1]
Description
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In the right conditions, Podozamites leaves sensu stricto preserve delicate cuticle and insect damage, and are thought to have been regularly shed. They are associated with conifer cones of the genera Swedenborgia, Cycadocarpidium, and Krassilovia.[2]
Podozamites leaves are strap-shaped or oblong, with smoothly parallel sides and dense longitudinal veins. They attach to a slender branch in a helical pattern, but twist into a distichous orientation (lying in a single plane along the branch). Both the upper (adaxial) and lower (abaxial) surfaces of the leaf have cells arranged into longitudinal bands. Some bands on the abaxial surface host broad stomata which are paracytic (with a subsidiary cell lateral to and paralleling each guard cell in a stoma). This is similar to Gnetales and especially bennettitaleans, suggesting that they may be related to these groups.[3]
The Krassilovia cone is roughly spherical and consists of densley packed interlocking overlapping bract-scale complexes surrounding a central axis. The cone is thought to have disintegrated at maturity to release the winged seeds. By contrast, the Swedenborgia and Cycadocarpidium cones are elongate and are only loosely packed.[2]
Evolutionary history
editPodozamites sensu stricto has been suggested to be closely related to Telemachus/Heidiphyllum (seed cone/leaves respectively), a broad-leaved conifer known from the Triassic of Gondwana.[2] Podozamites sensu stricto first became widespread at mid-latitudes during the Late Triassic. During the Early Jurassic in East Asia, it formed almost monospecific assemblages where it was the dominant plant. Over the course of the Jurassic, the distribution shifted northwards in response to the drying of the lower latitudes, becoming restricted to between 60 and 30 degrees north by the Early Cretaceous. Podozamites senus stricto would become extinct during the Turonian stage of the Late Cretaceous, coincident with the arrival of flowering plants into the Siberian region.[1]
Species
editA number of species within the genus were listed by Fossilworks, as of May 2021[update]: Podozamites agardhianus, Podozamites distans, Podozamites lanceolatus, Podozamites longifolius, Podozamites mucronatus, Podozamites pinnatus and Podozamites schenki.[4] Agathis jurassica, initially identified as Podozamites lanceolatus, has also been placed in this genus.[5] Podozamites harrissii from the Early Cretaceous of Mongolia is associated with Krassilovia mongolica, while Podozamites schenkii is associated with the Triassic-Jurassic Swedenborgia cryptomerioides and Triassic Cycadocarpidium erdmanni.[2] It has been noted that extant Agathis (Araucariaceae) and Nageia (Podocarpaceae) qualify as members of Podozamites under its morphogenus sense.[1]
References
edit- ^ a b c d Pole, Mike; Wang, Yongdong; Bugdaeva, Eugenia V.; Dong, Chong; Tian, Ning; Li, Liqin; Zhou, Ning (December 2016). "The rise and demise of Podozamites in east Asia—An extinct conifer life style". Palaeogeography, Palaeoclimatology, Palaeoecology. 464: 97–109. Bibcode:2016PPP...464...97P. doi:10.1016/j.palaeo.2016.02.037.
- ^ a b c d Herrera, Fabiany; Shi, Gongle; Mays, Chris; Ichinnorov, Niiden; Takahashi, Masamichi; Bevitt, Joseph J.; Herendeen, Patrick S.; Crane, Peter R. (2020-01-15). Peppe, Daniel (ed.). "Reconstructing Krassilovia mongolica supports recognition of a new and unusual group of Mesozoic conifers". PLOS ONE. 15 (1): e0226779. Bibcode:2020PLoSO..1526779H. doi:10.1371/journal.pone.0226779. ISSN 1932-6203. PMC 6961850. PMID 31940374.
- ^ Shi, Gongle; Herrera, Fabiany; Herendeen, Patrick S.; Leslie, Andrew B.; Ichinnorov, Niiden; Takahashi, Masamichi; Crane, Peter R. (2018-01-26). "Leaves of Podozamites and Pseudotorellia from the Early Cretaceous of Mongolia: stomatal patterns and implications for relationships". Journal of Systematic Palaeontology. 16 (2): 111–137. Bibcode:2018JSPal..16..111S. doi:10.1080/14772019.2016.1274343. ISSN 1477-2019. S2CID 90523531.
- ^ "†Podozamites Braun 1843 (conifer)". Paleobiology Database. Retrieved 2021-05-17.
- ^ Frese, M.; Gloy, G.; Oberprieler, R.G. & Gore, D.B. (2017). "Imaging of Jurassic fossils from the Talbragar Fish Bed using fluorescence, photoluminescence, and elemental and mineralogical mapping". PLOS ONE. 12 (6): e0179029. Bibcode:2017PLoSO..1279029F. doi:10.1371/journal.pone.0179029. PMC 5459505. PMID 28582427.