Pleuromeia is an extinct genus of lycophytes related to modern quillworts (Isoetes). Pleuromeia dominated vegetation during the Early Triassic all over Eurasia and elsewhere, in the aftermath of the Permian–Triassic extinction event. During this period it often occurred in monospecific assemblages. Its sedimentary context in monospecific assemblages on immature paleosols, is evidence that it was an opportunistic pioneer plant that grew on mineral soils with little competition.[1] It spread to high latitudes with greenhouse climatic conditions.[2]
| Pleuromeia Temporal range:
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|---|---|
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| Whole plant reconstruction of Pleuromeia sternbergi | |
Scientific classification 
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| Kingdom: | Plantae |
| Clade: | Tracheophytes |
| Clade: | Lycophytes |
| Class: | Lycopodiopsida |
| Order: | Isoetales |
| Family: | †Pleuromeiaceae |
| Genus: | †Pleuromeia Corda (1852) |
| Type species | |
| Sigillaria sternbergi Corda, 1839
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| Species | |
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See text | |
| Synonyms | |
|
Lycomeia | |
Description
editPleuromeia consisted of a single unbranched stem of variable thickness, which could grow to a maximum of 2 metres (6.6 ft) high in P. sternbergi, (though they were typically smaller),[3] with P. jiaochengensis only reaching about 30 centimetres (0.98 ft) in height.[4] Around the stem were helically arranged triangular leaves, which became tapered towards their ends. These were attached to rhomboidal-shaped leaf bases on the stem.[3] It had a 2-4 lobed bulbous base to which numerous adventive roots were attached. Pleuromeia produced a single heterosporus large cone (strobilus) at the tip of the stem or in some species many smaller cones. The top of the cone carries microsporophylls, the lower part megasporophylls, and both types may be intercalated midlength. Sporophylls are disposed from the bottom up. Both types are obovate, with a round to ovoid sporangium and a tongue-like extension nearer to the tip on the upper/inner side. The trilete microspores are hollow, round and 30–40 μm in diameter. Megaspores have a layered outer skin with a small trilete mark, are also hollow, round to ovoid and up to 300–400 μm in diameter.[5] The megaspores and microspores are assigned to Trileites and Densoisporites respectively.[3]
Ecology
editDense populations of Pleuromeia, in the aftermath of Permian–Triassic extinction event, are recorded around the world from habitats ranging from semi-arid to tidal.[6] Analysis suggest that they were perennial plants with relatively slow growth rates. However it is likely that they were also capable of rapid growth shortly prior to reproduction at the end of their lifespan. Their spores were likely able to survive long periods of dormancy, forming spore banks in the soil that were able to germinate long after the parent plants had died. Like modern quillworts, it has been suggested that Pleuromeia had Crassulacean acid metabolism (CAM)-type carbon fixation and/or used the Lycopsid Photosynthetic Pathway, as well intaking carbon dioxide from its roots. It is likely that while Pleuromeia was stress tolerant, it was poorly competitive against other plants under less stressed growing conditions, which may have been due to the much lower efficiency of the CAM-type carbon fixation compared to the typical C3 type used by other plants.[3]
Taxonomy
editWhen the Cathedral of Magdeburg was under repair during the 1830s, a block of sandstone crashed and split open, revealing a fragment of the stem of Pleuromeia sternbergi. This was described by George Graf zu Munster in 1839 as a species of Sigillaria. Corda later assigned the species to the new genus Pleuromeya. The sandstone had been mined in a quarry near Bernburg (Saale) where later on numerous specimens of Pleuromeia were found, including cones. P. sternbergi has since been found in other Lower and Middle Buntsandstein deposits elsewhere in Germany, France and Spain. Other species have been described from several localities in Russia, Australia, South America and Japan.[7]
Pleuromeia is placed in the family Pleuromeiaceae within the Isoetales, closely related to Isoetaceae, the family which contains modern Isoetes.[5] Around 20 species of Pleuromeia have been described, predominantly from the Northern Hemisphere, though it is not clear that all of these species are valid.[4]
Table of species after Deng et al. 2023.[4]
| Species | Age |
|
|---|---|---|
| Pleuromeia altinis | Induan | North China |
| Pleuromeia epicharis | Olenekian | North China |
| Pleuromeia hataii | Olenekian | Japan |
| Pleuromeia jiaochengensis | Induan | North China |
| Pleuromeia jokunzhica | Olenekian - Anisian | Darvaz, Kazakhstan |
| Pleuromeia longicaulis (Cylostrobus sydneyensis) | Lower Triassic | Eastern Australia |
| Pleuromeia marginulata | Anisian | South China |
| Pleuromeia obovata | Ladinian | North China |
| Pleuromeia olenekensis | Olenekian | Siberia (Russia) |
| Pleuromeia pateriformis | Induan | North China |
| Pleuromeia reniformis | Olenekian | Eastern Australia |
| Pleuromeia rossica | Olenekian | Upper Volga, Russia |
| Pleuromeia sanxiaensis | Anisian | South China |
| Pleuromeia shaolinii | Anisian | Northeast China |
| Pleuromeia sternbergii | Olenekian to Ladinian? | Across Eurasia (from Western Europe to China) and possibly Argentina |
| Pleuromeia sp. 1[8] | Olenekian | Taimyr, Russia |
| Pleuromeia sp. 2[9] | Olenekian | Nevada, USA |
The placement of the species Pleuromeia dubia from the Early Triassic of Australia in the genus has been questioned, due to its anatomy strongly differing from the typical species of the genus.[4]
Evolutionary history
editThe earliest members of the genus are known from the earliest Triassic (Induan) of North China, with the genus becoming abundant and globally distributed during the following Olenekian. During the Anisian, the genus declined following the development of a more warm humid climate and the subsequent diversification of other plant groups, with the youngest records of the genus being from the early Ladinian of North China, around 241.0-241.6 million years ago, with the genus likely being extinct by the beginning of the Late Triassic.[4]
References
edit- ^ Retallack, Gregory J. (1997). "Earliest Triassic origin of Isoetes and quillwort evolutionary radiation". Journal of Paleontology. 7 (3): 500–521. doi:10.1017/S0022336000039524. S2CID 140566050.
- ^ Retallack, Gregory J. (2013). "Permian and Triassic greenhouse crises". Gondwana Research. 24 (1): 90–103. Bibcode:2013GondR..24...90R. doi:10.1016/j.gr.2012.03.003.
- ^ a b c d Looy, Cindy V.; van Konijnenburg-van Cittert, Johanna H. A.; Duijnstee, Ivo A. P. (2021). "Proliferation of Isoëtalean Lycophytes During the Permo-Triassic Biotic Crises: A Proxy for the State of the Terrestrial Biosphere". Frontiers in Earth Science. 9: 55. Bibcode:2021FrEaS...9...55L. doi:10.3389/feart.2021.615370. ISSN 2296-6463.
- ^ a b c d e Deng, Shenghui; Lu, Yuanzheng; Fan, Ru; Ma, Xueying; Lyu, Dan; Luo, Zhong; Sun, Yanqi (December 2022). "A new species of Pleuromeia (Lycopsid) from the upper Middle Triassic of Northern China and discussion on the spatiotemporal distribution and evolution of the genus". Geobios. 75: 1–15. doi:10.1016/j.geobios.2022.10.001.
- ^ a b Naugolnykh, Serge V. (2013). "The heterosporous lycopodiophyte Pleuromeia rossica Neuburg, 1960 from the Lower Triassic of the Volga River basin (Russia): organography and reconstruction according to the 'Whole-Plant' concept" (PDF). Wulfenia. 20: 1–16.
- ^ Looy, C.V.; Van Konijnenburg-Van Cittert, J.H.A.; Visscher, H. (2000). "On the ecological success of isoetalean lycopsids after the end-Permian biotic crisis". LPP Contributions. 13: 63–70. Archived from the original on 2016-03-03. Retrieved 2009-05-13.
- ^ Bill Chaloner; Geoff Creber Royal Holloway. "An unexpected exposure: Pleuromeia". International Organisation of Palaeobotany. Retrieved 2015-03-19.
- ^ N.K. Mogutcheva Flora from the Induan Stage (Lower Triassic) of Middle Siberia Stratigr. Geol. Correl., 24 (2016), pp. 252-266
- ^ Mendelin, Morris; Schneebeli-Hermann, Elke; Kustatscher, Evelyn; Nowak, Hendrik; Vérard, Christian; Bucher, Hugo (July 2022). "An Early Triassic Pleuromeia strobilus from Nevada, USA". Review of Palaeobotany and Palynology. 302: 104663. doi:10.1016/j.revpalbo.2022.104663. hdl:20.500.11850/546721. ISSN 0034-6667.