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Silurian-Devonian Terrestrial Revolution

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Artist interpretation of a Devonian swamp forest scene. Artwork by Eduard Riou from The World Before the Deluge 1872

The Silurian-Devonian Terrestrial Revolution, also known as the Devonian Plant Explosion (DePE)[1] and the Devonian explosion, was a period of rapid colonization, diversification and radiation of land plants and fungi on dry lands that occurred 428 to 359 million years ago (Mya) during the Silurian and Devonian periods,[2][3][4] with the most critical phase occurring during the Late Silurian and Early Devonian.[5]

This diversification of terrestrial photosynthetic florae had vast impacts on the biotic composition of the Earth's surface, especially upon the Earth's atmosphere by oxygenation and carbon fixation. Their roots also eroded into the rocks, creating a layer of water-holding and mineral/organic matter-rich soil on top of Earth's crust known as the pedosphere, and significantly altering the chemistry of Earth's lithosphere and hydrosphere. The floral activities following the Silurian-Devonian plant revolution also exerted significant influences on changes in the water cycle and global climate, as well as driving the biosphere by creating diverse layers of vegetations that provide both sustenance and refuge for both upland and wetland habitats, paving the way for all terrestrial and aquatic biomes that would follow.[6]

Through fierce competition for sunlight, soil nutrients and available land space, phenotypic diversity of plants increased greatly during the Silurian and Devonian periods, comparable in scale and effect to the explosion in diversity of animal life during the Cambrian explosion,[7] especially in vertical growth of vascular plants, which allowed for expansive canopies to develop, and forever altering the plant evolutions that followed. As plants evolved and radiated, so did arthropods, who became the first established terrestrial animals and some formed symbiotic coevolution with plants.[8] Herbivory, granivory and detritivory subsequently evolved independently among terrestrial arthropods (especially hexapods such as insects, as well as myriapods), molluscs (land snails and slugs) and tetrapod vertebrates, causing plants to in turn develop defenses against foraging by animals.

The Silurian and Devonian terrestrial florae were largely spore-bearing plants (ferns) and significantly different in appearance, anatomy and reproductive strategies to most modern florae, which are dominated by fleshy seed-bearing angiosperms that evolved much later during the Early Cretaceous. Much of these Silurian-Devonian florae had died out in extinction events including the Kellwasser event, the Hangenberg event, the Carboniferous rainforest collapse, and the End-Permian extinction.[9][10]

Silurian and Devonian life

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Rather than plants, it was fungi, in particular nematophytes such as Prototaxites, that dominated the early stages of this terrestrial biodiversification event. Nematophytes towered over even the largest land plants during the Silurian and Early Devonian, only being truly surpassed in size in the Early Carboniferous. The nutrient-distributing glomeromycotan mycorrhizal networks of nematophytes were very likely to have acted as facilitators for the expansion of plants into terrestrial environments, which followed the colonising fungi.[11] The first fossils of arbuscular mycorrhizae, a type of symbiosis between fungi and vascular plants, are known from the Early Devonian.[12]

Land plants probably evolved in the Ordovician.[13] The earliest radiations of the first land plants, also known as embryophytes, were bryophytes, which began to transform terrestrial environments and the global climate in the Ordovician.[14][15][16] Baltica was a particularly important cradle for early land plant evolution, with it having a diverse flora by the Darriwilian.[17] ∆199Hg and ∆200Hg excursions reveal that land plants had already spread across much of the Earth's land surface by the Early Silurian.[18] The end of the Homerian glaciation, a glacial phase of the Early Palaeozoic Ice Age, and the corresponding period of global warming marked the first major diversification of plants that produced trilete spores. The later glaciation during the middle Ludfordian, corresponding to the Lau event, led to a major marine regression, creating significant areas of new dry land habitat that were colonised by plants, along with cyanobacterial mats. These newly created terrestrial habitats helped facilitate the global expansion and evolutionary radiation of polysporangiophytes.[19] A warming climate during the subsequent Pridoli epoch lent itself to further floral diversification.[20] During the Wenlock epoch of the Silurian, the first fossils of vascular plants appear in the fossil record in the form of sporophytes of polysporangiophytes.[21] Lycophytes first appeared during the later Ludlow epoch in the form of Baragwanathia,[22] which was an aquatic predecessor of fully terrestrialised lycophytes.[23] Palynological evidence points to Silurian terrestrial floras exhibiting little provincialism relative to present day floras that vary significantly by region, instead being broadly similar across the globe.[24] Plant diversification in the Silurian was aided by the presence of numerous small, rapidly changing volcanic islands in the Rheic Ocean that acted as natural laboratories accelerating evolutionary changes and enabling distinct, endemic floral lineages to arise.[25] Silurian plants rarely reached large sizes, with heights of 13 cm, achieved by Tichavekia grandis, being exceptionally large for the time.[26]

The Devonian witnessed the widespread greening of the Earth's surface,[27] with many modern vascular plant clades originating during this period. Basal members of Euphyllophytina, the clade that includes trimerophytes, ferns, progymnosperms, and seed plants, are known from Early Devonian fossils.[28] Lycopsids experienced their first evolutionary radiation during the Devonian period.[13] Early Devonian plant communities were generally similar regardless of what landmass they inhabited,[29] although zosterophyllopsids displayed high levels of endemism.[30]

In the Middle Devonian, euphyllophytes continued to increase in diversity.[31] The first true forest environments featuring trees exceeding eight metres in height emerged by the Middle Devonian,[32] with the earliest known fossil forest dating to the Eifelian.[33] The oldest known trees were members of the clade Cladoxylopsida.[34] Devonian swamp forests were dominated by giant horsetails (Equisetales), clubmosses, ancestral ferns (pteridophytes), and large lycophyte vascular plants such as Lepidodendrales, referred to as scale trees for the appearance of scales on their photosynthetic trunks. These lycophytes, which could grow up to 40 metres high, grew in great numbers around swamps along with tracheophytes.[9] Seed ferns and true leaf-bearing plants such as progymnosperms also appeared at this time and became dominant in many habitats, particularly archeopteridaleans, which were likely related to conifers.[35] Pseudosporochnaleans (morphologically similar to palms and tree ferns) likewise experienced a similar rise to dominance.[36] Archeopteridaleans had likely developed extensive root systems, making them resistant to drought, and meaning they had a more significant impact on Devonian soil environments than pseudosporochnaleans.[37]

The Late Devonian saw the most rapid land plant diversification of the Devonian, largely owing to the rapid radiation of pteridophytes and progymnosperms.[38] Cladoxylopsids continued to dominate forest ecosystems during the early Late Devonian.[34] During the latest Devonian, the first true spermatophytes appeared, evolving as a sister group to archaeopteridaleans or to progymnosperms as a whole.[39]

Most flora in Devonian coal swamps would have seemed alien in appearance when compared with modern flora, such as giant horsetails which could grow up to 30 m in height. Devonian ancestral plants of modern plants that may have been very similar in appearance are ferns (Polypodiopsida), although many of them are thought to have been epiphytes rather than grounded plants. True gymnosperms like ginkgos (Ginkgophyta) and cycads (Cycadophyta) would appear slightly after the Devonian in the Carboniferous.[9]

Vascular plant lineages of sphenoids, fern, progymnosperms, and seed plants evolved laminated leaves during the Devonian. Plants that possessed true leaves appeared during the Devonian, though they may have many independent origins with parallel trajectories of leaf morphologies. Morphological evidence to support this diversification theory appears in the Late Devonian or Early Carboniferous when compared with modern leaf morphologies. The marginal meristem also evolved in a parallel fashion through a similar process of modified structures around this time period.[40] In a 1994 study by Richard M Bateman and William A. Dimechele of the evolutionary history of heterospory in the plant kingdom, researchers found evidence of 11 origins of heterospory events that had occurred independently in the Devonian within Zosterophyllopsida, Sphenopsida, Progymnospermopsida. The effect of this heterospory was that it presented a primary evolutionary advantage for these plants in colonizing land.[41] The simultaneous colonization of dry land and increase in plant body size that many lineages underwent during this time was likely facilitated by another parallel development: the replacement of the ancestral central cylinder of xylem with more elongate, complex xylem strand shapes that would have made the plant body more resistant to the spread of drought-induced embolism.[42] Tracheids, tapered cells that make up the xylem of vascular plants, first appear in the fossil record during the Early Devonian.[32] Woody stems evolved during the Devonian as well, with the first evidence of them dating back to the Early Devonian.[43] Evidence of root structures appears for the first time during the Late Silurian.[44] Further appearances of roots in the fossil record are found in Early Devonian lycophytes,[45] and it has been suggested that the development of roots was an adaptation for maximising water acquisition in response to the increase in aridity over the course of the Silurian and Devonian.[46] The Early Devonian also saw the appearance of complex subterranean rhizome networks.[47]


Effect on atmosphere, soil, and climate

[edit]

Deep-rooted vascular plants had drastic impacts upon soil, atmosphere, and oceanic oxygen composition. The Devonian Plant Hypothesis is an explanation about these effects upon biogeomorphic ecosystems of climate and marine environments.[6] A climate/carbon/vegetation model could explain the effects of plant colonization during the Devonian. Expansion of terrestrial Devonian flora modified soil properties, increasing silicate weathering by way of rhizosphere development as evidenced by pedogenic carbonates.[48][49] This caused atmospheric CO2 levels to fall from around 6300 to 2100 ppmv, although it also drastically reduced the albedo of much of Earth's land surface, retarding the cooling effects of this greenhouse gas drawdown.[50] The biological sequestration of so much carbon dioxide resulted in the beginning of the Late Palaeozoic Ice Age at the terminus of the Devonian,[51][52][53] together with the tectonic uplift of the continent Gondwana.[54]

Oxygen levels rose as a direct result of plant expansion.[50] With increased oxygenation came increased fire activity.[55] Earth's atmosphere first became sufficiently high in oxygen to produce wildfires in the Pridoli, when the first charcoal evidence of wildfires is recorded.[56] For most of the Early and Middle Devonian, the atmosphere was insufficiently oxygenated to enable significant fire activity.[57] By the late Famennian, however, oxygen levels were high enough to enable wildfires to occur with regularity and on large scales,[58] something which had not been previously possible due to the paucity of atmospheric oxygen.[59]

The rise of trees and forests caused greater amounts of fine sediment particles to be retained on alluvial plains, increasing the complexity of meandering and braided fluvial systems. The greater complexity of terrestrial habitats facilitated the colonisation of the land by arthropods. Additionally, the increased weathering of phosphates and quantity of terrestrial humic matter increased nutrient levels in freshwater lakes, facilitating their colonisation by freshwater vertebrates. From these lakes, vertebrates would later follow arthropods in their conquest of the land.[60]

The Devonian explosion had global consequences on oceanic nutrient content and sediment cycling, which had led to the Devonian mass extinction. The expansion of trees in the Late Devonian drastically increased biological weathering rates and the consequent riverine input of nutrients into the ocean.[61][62][63] The altering of soil composition created anoxic sedimentation (or black shales), oceanic acidification, and global climate changes. This led to harsh living conditions for oceanic and terrestrial life.[64]

The increase in terrestrial plant matter in swamplands explains the deposits of coal and oil that would later characterize the Carboniferous.[9]

References

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  1. ^ Pawlik, Łukasz; Buma, Brian; Šamonil, Pavel; Kvaček, Jiří; Gałązka, Anna; Kohout, Petr; Malik, Ireneusz (June 2020). "Impact of trees and forests on the Devonian landscape and weathering processes with implications to the global Earth's system properties - A critical review". Earth-Science Reviews. 205: 103200. Bibcode:2020ESRv..20503200P. doi:10.1016/j.earscirev.2020.103200. hdl:20.500.12128/14041. S2CID 218933989.
  2. ^ Capel, Elliot; Cleal, Christopher J.; Xue, Jinzhuang; Monnet, Claude; Servais, Thomas; Cascales-Miñana, Borja (August 2022). "The Silurian–Devonian terrestrial revolution: Diversity patterns and sampling bias of the vascular plant macrofossil record". Earth-Science Reviews. 231: 104085. Bibcode:2022ESRv..23104085C. doi:10.1016/j.earscirev.2022.104085. hdl:20.500.12210/76731.
  3. ^ Xue, Jinzhuang; Huang, Pu; Wang, Deming; Xiong, Conghui; Liu, Le; Basinger, James F. (May 2018). "Silurian-Devonian terrestrial revolution in South China: Taxonomy, diversity, and character evolution of vascular plants in a paleogeographically isolated, low-latitude region". Earth-Science Reviews. 180: 92–125. Bibcode:2018ESRv..180...92X. doi:10.1016/j.earscirev.2018.03.004. Retrieved 8 November 2022.
  4. ^ Capel, Elliot; Cleal, Christopher J.; Gerrienne, P.; Servais, Thomas; Cascales-Miñana, Borja (15 March 2021). "A factor analysis approach to modelling the early diversification of terrestrial vegetation". Palaeogeography, Palaeoclimatology, Palaeoecology. 566: 110170. Bibcode:2021PPP...56610170C. doi:10.1016/j.palaeo.2020.110170. hdl:20.500.12210/55336. S2CID 230591548. Retrieved 8 November 2022.
  5. ^ Hao, Shougang; Xue, Jinzhuang; Liu, Zhenfeng; Wang, Deming (May 2007). "Zosterophyllum Penhallow around the Silurian-Devonian Boundary of Northeastern Yunnan, China". International Journal of Plant Sciences. 168 (4): 477–489. doi:10.1086/511011. S2CID 83631931. Retrieved 12 November 2022.
  6. ^ a b Pawlik, Łukasz; Buma, Brian; Šamonil, Pavel; Kvaček, Jiří; Gałązka, Anna; Kohout, Petr; Malik, Ireneusz (June 2020). "Impact of trees and forests on the Devonian landscape and weathering processes with implications to the global Earth's system properties - A critical review". Earth-Science Reviews. 205: 103200. Bibcode:2020ESRv..20503200P. doi:10.1016/j.earscirev.2020.103200. hdl:20.500.12128/14041.
  7. ^ Bateman, Richard M.; Crane, Peter R.; DiMichele, William A.; Kenrick, Paul R.; Rowe, Nick P.; Speck, Thomas; Stein, William E. (November 1998). "Early Evolution of Land Plants: Phylogeny, Physiology, and Ecology of the Primary Terrestrial Radiation". Annual Review of Ecology and Systematics. 29: 263–292. doi:10.1146/annurev.ecolsys.29.1.263. Retrieved 26 December 2022.
  8. ^ Labandeira, Conrad (30 October 2006). "Silurian to Triassic Plant and Hexapod Clades and their Associations: New Data, a Review, and Interpretations" (PDF). Arthropod Systematics & Phylogeny. 63 (1): 53–94. doi:10.3897/asp.64.e31644. Retrieved 23 January 2023.
  9. ^ a b c d Cruzan, Mitchell (2018). Evolutionary Biology A Plant Perspective. New York: Oxford University Press. pp. 37–39. ISBN 978-0-19-088267-9.
  10. ^ Cascales-Miñana, B.; Cleal, C. J. (2011). "Plant fossil record and survival analyses". Lethaia. 45: 71–82. doi:10.1111/j.1502-3931.2011.00262.x.
  11. ^ Retallack, Gregory J. (June 2022). "Ordovician-Devonian lichen canopies before evolution of woody trees". Gondwana Research. 106: 211–223. Bibcode:2022GondR.106..211R. doi:10.1016/j.gr.2022.01.010. S2CID 246320087. Retrieved 22 November 2022.
  12. ^ Lutzoni, François; Nowak, Michael D.; Alfaro, Michael E.; Reeb, Valérie; Miadlikowska, Jolanta; Krug, Michael; Arnold, A. Elizabeth; Lewis, Louise A.; Swofford, David L.; Hibbett, David; Hilu, Khidir; James, Timothy Y.; Quandt, Dietmar; Magallón, Susana (21 December 2018). "Contemporaneous radiations of fungi and plants linked to symbiosis". Nature Communications. 9 (1): 5451. Bibcode:2018NatCo...9.5451L. doi:10.1038/s41467-018-07849-9. PMC 6303338. PMID 30575731.
  13. ^ a b Feng, Zhuo (11 September 2017). "Late Palaeozoic plants". Current Biology. 27 (17): R905–R909. doi:10.1016/j.cub.2017.07.041. PMID 28898663.
  14. ^ Lenton, Timothy M.; Crouch, Michael; Johnson, Martin; Pires, Nuno; Dolan, Liam (1 February 2012). "First plants cooled the Ordovician". Nature Geoscience. 5 (2): 86–89. Bibcode:2012NatGe...5...86L. doi:10.1038/ngeo1390. ISSN 1752-0908. Retrieved 18 October 2022.
  15. ^ Adiatma, Y. Datu; Saltzman, Matthew R.; Young, Seth A.; Griffith, Elizabeth M.; Kozik, Nevin P.; Edwards, Cole T.; Leslie, Stephen A.; Bancroft, Alyssa M. (15 November 2019). "Did early land plants produce a stepwise change in atmospheric oxygen during the Late Ordovician (Sandbian ~458 Ma)?". Palaeogeography, Palaeoclimatology, Palaeoecology. 534: 109341. Bibcode:2019PPP...53409341A. doi:10.1016/j.palaeo.2019.109341. S2CID 201309297.
  16. ^ Quinton, Page C.; Rygel, Michael C.; Heins, Megan (15 July 2017). "Sequence stratigraphy and carbon isotopes from the Trenton and Black River Groups near Union Furnace, PA: Constraining the role of land plants in the Ordovician world". Palaeogeography, Palaeoclimatology, Palaeoecology. 574: 110440. doi:10.1016/j.palaeo.2021.110440. ISSN 0031-0182. S2CID 235577811. Retrieved 17 October 2023.
  17. ^ Rubinstein, Claudia V.; Vajda, Vivi (24 July 2019). "Baltica cradle of early land plants? Oldest record of trilete spores and diverse cryptospore assemblages; evidence from Ordovician successions of Sweden". Geologiska Föreningens Förhandlingar. 141 (3): 181–190. Bibcode:2019GFF...141..181R. doi:10.1080/11035897.2019.1636860. hdl:11336/124409. ISSN 1103-5897.
  18. ^ Yuan, Wei; Liu, Mu; Chen, Daizhao; Xing, Yao-Wu; Spicer, Robert A.; Chen, Jitao; Them, Theodore R.; Wang, Xun; Li, Shizhen; Guo, Chuan; Zhang, Gongjing; Zhang, Liyu; Zhang, Hui; Feng, Xinbin (28 April 2023). "Mercury isotopes show vascular plants had colonized land extensively by the early Silurian". Science Advances. 9 (17): eade9510. Bibcode:2023SciA....9E9510Y. doi:10.1126/sciadv.ade9510. ISSN 2375-2548. PMC 10146902. PMID 37115923.
  19. ^ Pšenička, Josef; Bek, Jiří; Frýda, Jiří; Žárský, Viktor; Uhlířová, Monika; Štorch, Petr (31 August 2022). "Dynamics of Silurian Plants as Response to Climate Changes". Life. 11 (9): 906. doi:10.3390/life11090906. PMC 8470493. PMID 34575055.
  20. ^ Bek, Jiří; Štorch, Petr; Tonarová, Petra; Libertín, Milan (2022). "Early Silurian (mid-Sheinwoodian) palynomorphs from the Loděnice-Špičatý vrch, Prague Basin, Czech Republic". Bulletin of Geosciences. 97 (3): 385–396. doi:10.3140/bull.geosci.1831. S2CID 252148763.
  21. ^ Libertín, Milan; Kvaček, Jiří; Bek, Jiří; Žárský, Viktor; Štorch, Petr (30 April 2018). "Sporophytes of polysporangiate land plants from the early Silurian period may have been photosynthetically autonomous". Nature Plants. 4 (5): 269–271. doi:10.1038/s41477-018-0140-y. PMID 29725100. S2CID 256679794. Retrieved 9 November 2022.
  22. ^ Rickards, R. B. (1 March 2000). "The age of the earliest club mosses: the Silurian Baragwanathia flora in Victoria, Australia". Geological Magazine. 137 (2): 207–209. Bibcode:2000GeoM..137..207R. doi:10.1017/S0016756800003800. S2CID 131287538. Retrieved 11 November 2022.
  23. ^ Kraft, Petr; Kvaček, Zlatko (May 2017). "Where the lycophytes come from? – A piece of the story from the Silurian of peri-Gondwana". Gondwana Research. 45: 180–190. doi:10.1016/j.gr.2017.02.001. Retrieved 16 June 2024 – via Elsevier Science Direct.
  24. ^ Césari, Silvia N.; Marenssi, Sergio; Limarino, Carlos O.; Ciccioli, Patricia L.; Bello, Fanny C.; Ferreira, Luis C.; Scarlatta, Leonardo R. (1 December 2020). "The first upper Silurian land-derived palynological assemblage from South America: Depositional environment and stratigraphic significance". Palaeogeography, Palaeoclimatology, Palaeoecology. 559: 109970. Bibcode:2020PPP...55909970C. doi:10.1016/j.palaeo.2020.109970. S2CID 225020262. Retrieved 11 November 2022.
  25. ^ Kraft, Petr; Pšenička, Josef; Sakala, Jakub; Frýda, Jiří (15 January 2019). "Initial plant diversification and dispersal event in upper Silurian of the Prague Basin". Palaeogeography, Palaeoclimatology, Palaeoecology. 514: 144–155. Bibcode:2019PPP...514..144K. doi:10.1016/j.palaeo.2018.09.034. S2CID 133777180. Retrieved 9 November 2022.
  26. ^ Uhlířová, Monika; Pšenička, Josef; Sakala, Jakub; Bek, Jiří (March 2022). "A study of the large Silurian land plant Tichavekia grandis Pšenička et al. from the Požáry Formation (Czech Republic)". Review of Palaeobotany and Palynology. 298: 104587. Bibcode:2022RPaPa.29804587U. doi:10.1016/j.revpalbo.2021.104587. S2CID 245295312. Retrieved 11 November 2022.
  27. ^ Shen, Zhen; Monnet, Claude; Cascales-Miñana, Borja; Gong, Yiming; Dong, Xianghong; Kroeck, David M.; Servais, Thomas (January 2020). "Diversity dynamics of Devonian terrestrial palynofloras from China: Regional and global significance". Earth-Science Reviews. 200: 102967. Bibcode:2020ESRv..20002967S. doi:10.1016/j.earscirev.2019.102967. hdl:20.500.12210/34284. S2CID 210618841. Retrieved 22 November 2022.
  28. ^ Xu, Hong-He; Wang, Yi; Tang, Peng; Fu, Qiang; Wang, Yao (1 October 2019). "Discovery of Lower Devonian plants from Jiangxi, South China and the pattern of Devonian transgression after the Kwangsian Orogeny in the Cathaysia Block". Palaeogeography, Palaeoclimatology, Palaeoecology. 531: 108982. Bibcode:2019PPP...53108982X. doi:10.1016/j.palaeo.2018.11.007. S2CID 133712540. Retrieved 12 November 2022.
  29. ^ Xu, Hong-He; Yang, Ning; Bai, Jiao; Wang, Yao; Liu, Feng; Ouyang, Shu (1 February 2022). "Palynological assemblage of the Lower Devonian of Hezhang, Guizhou, southwestern China". Review of Palaeobotany and Palynology. 297: 104561. Bibcode:2022RPaPa.29704561X. doi:10.1016/j.revpalbo.2021.104561. ISSN 0034-6667. S2CID 244048051. Retrieved 25 November 2023.
  30. ^ Cascales-Miñana, Borja; Meyer-Berthaud, Brigitte (1 April 2015). "Diversity patterns of the vascular plant group Zosterophyllopsida in relation to Devonian paleogeography". Palaeogeography, Palaeoclimatology, Palaeoecology. 423: 53–61. doi:10.1016/j.palaeo.2015.01.024. Retrieved 20 May 2024 – via Elsevier Science Direct.
  31. ^ Toledo, Selin; Bippus, Alexander C.; Atkinson, Brian A.; Bronson, Allison W.; Tomescu, Alexandru M. F. (25 May 2021). "Taxon sampling and alternative hypotheses of relationships in the euphyllophyte plexus that gave rise to seed plants: insights from an Early Devonian radiatopsid". New Phytologist. 232 (2): 914–927. doi:10.1111/nph.17511. PMID 34031894. S2CID 235199240.
  32. ^ a b Hibbett, David; Blanchette, Robert; Kenrick, Paul; Mills, Benjamin (11 July 2016). "Climate, decay, and the death of the coal forests". Current Biology. 26 (13): R563–R567. doi:10.1016/j.cub.2016.01.014. PMID 27404250.
  33. ^ Davies, Neil S.; McMahon, William J.; Berry, Christopher M. (23 February 2024). "Earth's earliest forest: fossilized trees and vegetation-induced sedimentary structures from the Middle Devonian (Eifelian) Hangman Sandstone Formation, Somerset and Devon, SW England". Journal of the Geological Society. doi:10.1144/jgs2023-204. ISSN 0016-7649. Retrieved 25 February 2024 – via GeoScienceWorld.
  34. ^ a b Xu, Hong-He; Berry, Christopher M.; Stein, William E.; Wang, Yi; Tang, Peng; Fu, Qiang (23 October 2017). "Unique growth strategy in the Earth's first trees revealed in silicified fossil trunks from China". Proceedings of the National Academy of Sciences of the United States of America. 114 (45): 12009–12014. Bibcode:2017PNAS..11412009X. doi:10.1073/pnas.1708241114. PMC 5692553. PMID 29078324. Retrieved 18 May 2023.
  35. ^ Stein, William E.; Berry, Christopher M.; Morris, Jennifer L.; Hernick, Linda VanAller; Mannolini, Frank; Ver Straeten, Charles; Landing, Ed; Marshall, John E. A.; Wellman, Charles H.; Beerling, David J.; Leake, Jonathan R. (3 February 2020). "Mid-Devonian Archaeopteris Roots Signal Revolutionary Change in Earliest Fossil Forests". Current Biology. 30 (3): 321–331. doi:10.1016/j.cub.2019.11.067. PMID 31866369. S2CID 209422168.
  36. ^ Berry, Christopher M.; Marshall, John E.A. (December 2015). "Lycopsid forests in the early Late Devonian paleoequatorial zone of Svalbard". Geology. 43 (12): 1043–1046. Bibcode:2015Geo....43.1043B. doi:10.1130/G37000.1. ISSN 1943-2682.
  37. ^ Meyer-Berthaud, B.; Soria, A.; Decombeix, A.-L. (2010). "The land plant cover in the Devonian: a reassessment of the evolution of the tree habit". Geological Society, London, Special Publications. 339 (1): 59–70. Bibcode:2010GSLSP.339...59M. doi:10.1144/SP339.6. ISSN 0305-8719. S2CID 129915170.
  38. ^ Salles, Tristan; Husson, Laurent; Lorcery, Manon; Hadler Boggiani, Beatriz (7 December 2023). "Landscape dynamics and the Phanerozoic diversification of the biosphere". Nature. 624 (7990): 115–121. Bibcode:2023Natur.624..115S. doi:10.1038/s41586-023-06777-z. ISSN 0028-0836. PMC 10700141. PMID 38030724. Retrieved 31 December 2023.
  39. ^ Wellman, Charles H. (31 December 2008). "Ultrastructure of dispersed and in situ specimens of the Devonian spore Rhabdosporites langii: evidence for the evolutionary relationships of progymnosperms". Palaeontology. 52 (1): 139–167. doi:10.1111/j.1475-4983.2008.00823.x. S2CID 128869785. Retrieved 25 December 2022.
  40. ^ Boyce, C.; Knoll, A. (2002). "Evolution of developmental potential and the multiple independent origins of leaves in Paleozoic vascular plants". Paleobiology. 28 (1): 70–100. doi:10.1666/0094-8373(2002)028<0070:EODPAT>2.0.CO;2. S2CID 1650492 – via DASH.
  41. ^ Bateman, Richard M.; DiMichele, William A. (August 1994). "Heterospory: The Most Iterative Key Innovation in the Evolutionary History of the Plant Kingdom". Biological Reviews. 69 (3): 345–417. doi:10.1111/j.1469-185X.1994.tb01276.x. ISSN 1464-7931. S2CID 29709953.
  42. ^ Bouda, Martin; Huggett, Brett A.; Prats, Kyra A.; Wason, Jay W.; Wilson, Jonathan P.; Brodersen, Craig R. (2022-11-11). "Hydraulic failure as a primary driver of xylem network evolution in early vascular plants". Science. 378 (6620): 642–646. Bibcode:2022Sci...378..642B. doi:10.1126/science.add2910. ISSN 0036-8075. PMID 36356120. S2CID 253458196.
  43. ^ Berbee, Mary L.; Strullu-Derrien, Christine; Delaux, Pierre-Marc; Strother, Paul K.; Kenrick, Paul; Selosse, Marc-André; Taylor, John W. (9 September 2020). "Genomic and fossil windows into the secret lives of the most ancient fungi". Nature Reviews Microbiology. 18 (12): 717–730. doi:10.1038/s41579-020-0426-8. PMID 32908302. S2CID 221622787. Retrieved 7 December 2022.
  44. ^ Kenrick, Paul; Crane, Peter R. (4 September 1997). "The origin and early evolution of plants on land". Nature. 389 (1): 33–39. Bibcode:1997Natur.389...33K. doi:10.1038/37918. S2CID 3866183. Retrieved 18 May 2023.
  45. ^ Matsunaga, Kelly K. S.; Tomescu, Alexandru M. F. (26 February 2016). "Root evolution at the base of the lycophyte clade: insights from an Early Devonian lycophyte". Annals of Botany. 117 (4): 585–598. doi:10.1093/aob/mcw006. PMC 4817433. PMID 26921730. Retrieved 18 May 2023.
  46. ^ Gurung, Khushboo; Field, Katie J.; Batterman, Sarah J.; Goddéris, Yves; Donnadieu, Yannick; Porada, Philipp; Taylor, Lyla L.; Mills, Benjamin J. W. (4 August 2022). "Climate windows of opportunity for plant expansion during the Phanerozoic". Nature Communications. 13 (1): 4530. Bibcode:2022NatCo..13.4530G. doi:10.1038/s41467-022-32077-7. PMC 9352767. PMID 35927259.
  47. ^ Xue, Jinzhuang; Deng, Zhenzhen; Huang, Pu; Huang, Kangjun; Benton, Michael James; Cui, Ying; Wang, Deming; Liu, Jianbo; Shen, Bing; Basinger, James F.; Hao, Shougang (8 August 2016). "Belowground rhizomes in paleosols: The hidden half of an Early Devonian vascular plant". Proceedings of the National Academy of Sciences of the United States of America. 113 (34): 9451–9456. Bibcode:2016PNAS..113.9451X. doi:10.1073/pnas.1605051113. PMC 5003246. PMID 27503883.
  48. ^ Retallack, Gregory J. (25 April 1997). "Early Forest Soils and Their Role in Devonian Global Change". Science. 276 (5312): 583–585. doi:10.1126/science.276.5312.583. PMID 9110975. Retrieved 23 July 2023.
  49. ^ Boyce, C. Kevin; Lee, Jung-Eun (30 August 2017). "Plant Evolution and Climate Over Geological Timescales". Annual Review of Earth and Planetary Sciences. 45 (1): 61–87. doi:10.1146/annurev-earth-063016-015629. ISSN 0084-6597. Retrieved 20 June 2024.
  50. ^ a b Le Hir, Guillaume; Donnadieu, Yannick; Goddéris, Yves; Meyer-Berthaud, Brigitte; Ramstein, Gilles; Blakey, Ronald C. (October 2011). "The climate change caused by the land plant invasion in the Devonian". Earth and Planetary Science Letters. 310 (3–4): 203–212. Bibcode:2011E&PSL.310..203L. doi:10.1016/j.epsl.2011.08.042.
  51. ^ Qie, Wenkun; Algeo, Thomas J.; Luo, Genming; Herrmann, Achim (1 October 2019). "Global events of the Late Paleozoic (Early Devonian to Middle Permian): A review". Palaeogeography, Palaeoclimatology, Palaeoecology. 531: 109259. Bibcode:2019PPP...53109259Q. doi:10.1016/j.palaeo.2019.109259. S2CID 198423364. Retrieved 23 December 2022.
  52. ^ Streel, Maurice; Caputo, Mário V.; Loboziak, Stanislas; Melo, José Henrique G. (November 2000). "Late Frasnian–Famennian climates based on palynomorph analyses and the question of the Late Devonian glaciations". Earth-Science Reviews. 52 (1–3): 121–173. Bibcode:2000ESRv...52..121S. doi:10.1016/S0012-8252(00)00026-X. Retrieved 28 January 2023.
  53. ^ Mintz, Jason S.; Driese, Steven G.; White, Joseph D. (1 January 2010). "Environmental and Ecological Variability of Middle Devonian (Givetian) Forests in Appalachian Basin Paleosols, New York, United States". PALAIOS. 25 (2): 85–96. Bibcode:2010Palai..25...85M. doi:10.2110/palo.2009.p09-086r. S2CID 130624914. Retrieved 2 August 2023.
  54. ^ Rosa, Eduardo L. M.; Isbell, John L. (2021). "Late Paleozoic Glaciation". In Alderton, David; Elias, Scott A. (eds.). Encyclopedia of Geology (2nd ed.). Academic Press. pp. 534–545. doi:10.1016/B978-0-08-102908-4.00063-1. ISBN 978-0-08-102909-1. S2CID 226643402.
  55. ^ Glasspool, Ian J.; Scott, Andrew C.; Waltham, David; Pronina, Natalia; Shao, Longyi (23 September 2015). "The impact of fire on the Late Paleozoic Earth system". Frontiers in Plant Science. 6: 756. doi:10.3389/fpls.2015.00756. ISSN 1664-462X. PMC 4585212. PMID 26442069.
  56. ^ Glasspool, I. J.; Edwards, D.; Axe, L. (1 May 2004). "Charcoal in the Silurian as evidence for the earliest wildfire". Geology. 32 (5): 381. Bibcode:2004Geo....32..381G. doi:10.1130/G20363.1. ISSN 0091-7613. Retrieved 17 October 2023.
  57. ^ Algeo, Thomas J.; Ingall, Ellery (6 December 2007). "Sedimentary Corg:P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2". Palaeogeography, Palaeoclimatology, Palaeoecology. Neoproterozoic to Paleozoic Ocean Chemistry. 256 (3): 130–155. Bibcode:2007PPP...256..130A. doi:10.1016/j.palaeo.2007.02.029. ISSN 0031-0182. Retrieved 12 December 2023 – via Elsevier Science Direct.
  58. ^ Marynowski, Leszek; Filipiak, Paweł; Zatoń, Michał (15 January 2010). "Geochemical and palynological study of the Upper Famennian Dasberg event horizon from the Holy Cross Mountains (central Poland)". Geological Magazine. 147 (4): 527–550. Bibcode:2010GeoM..147..527M. doi:10.1017/S0016756809990835. S2CID 140657109. Retrieved 24 March 2023.
  59. ^ Marynowski, Leszek; Filipak, Paweł (1 May 2007). "Water column euxinia and wildfire evidence during deposition of the Upper Famennian Hangenberg event horizon from the Holy Cross Mountains (central Poland)". Geological Magazine. 144 (3): 569–595. Bibcode:2007GeoM..144..569M. doi:10.1017/S0016756807003317. S2CID 129306243. Retrieved 28 January 2023.
  60. ^ Buatois, Luis A.; Davies, Neil S.; Gibling, Martin R.; Krapovickas, Verónica; Labandeira, Conrad C.; MacNaughton, Robert B.; Mángano, M. Gabriela; Minter, Nicholas J.; Shillito, Anthony P. (31 May 2022). "The Invasion of the Land in Deep Time: Integrating Paleozoic Records of Paleobiology, Ichnology, Sedimentology, and Geomorphology". Integrative and Comparative Biology. 62 (2): 297–331. doi:10.1093/icb/icac059. PMID 35640908. Retrieved 2 April 2023.
  61. ^ Dahl, Tais W.; Arens, Susanne K. M. (5 August 2020). "The impacts of land plant evolution on Earth's climate and oxygenation state – An interdisciplinary review". Chemical Geology. 547: 119665. Bibcode:2020ChGeo.54719665D. doi:10.1016/j.chemgeo.2020.119665. ISSN 0009-2541. S2CID 219484664. Retrieved 29 September 2023.
  62. ^ Smart, Matthew S.; Filippelli, Gabriel; Gilhooly III, William P.; Marshall, John E.A.; Whiteside, Jessica H. (9 November 2022). "Enhanced terrestrial nutrient release during the Devonian emergence and expansion of forests: Evidence from lacustrine phosphorus and geochemical records". Geological Society of America Bulletin. doi:10.1130/B36384.1. Retrieved 2 August 2023.
  63. ^ Algeo, T.J.; Scheckler, S. E. (1998). "Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events". Philosophical Transactions of the Royal Society B: Biological Sciences. 353 (1365): 113–130. doi:10.1098/rstb.1998.0195. PMC 1692181.
  64. ^ Becker, R. T.; Königshof, P.; Brett, C. E. (1 January 2016). "Devonian climate, sea level and evolutionary events: an introduction". Geological Society, London, Special Publications. 423 (1): 1–10. Bibcode:2016GSLSP.423....1B. doi:10.1144/SP423.15. ISSN 0305-8719.
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