Cretaceous Terrestrial Revolution

The Cretaceous Terrestrial Revolution (abbreviated KTR), also known as the Angiosperm Terrestrial Revolution (ATR) by authors who consider it to have lasted into the Palaeogene,[1] describes the intense floral diversification of flowering plants (angiosperms) and the coevolution of pollinating insects, as well as the subsequent faunal radiation of frugivorous, nectarivorous and insectivorous avians, mammals, lissamphibians and squamate reptiles during the Middle to Late Cretaceous, from around 125 Mya to 80 Mya.[2] Alternatively, according to Michael Benton, the ATR is proposed to have lasted from 100 Ma, when the first highly diverse angiosperm leaf floras are known, to 50 Ma, during the Early Eocene Climatic Optimum, by which point most crown lineages of angiosperms had evolved.[1] The KTR was enabled by the dispersed positions of the continents and the formation of new oceans during the Cretaceous in the aftermath of Pangaea's breakup in the preceding Jurassic period, which enhanced the hydrological cycle and promoted the expansion of temperate climatic zones, fuelling radiations of angiosperms.[3]

Before Lloyd et al.'s 2008 paper described the KTR, it had been widely accepted in paleontology that new families of dinosaurs evolved during the Middle to Late Cretaceous, including the euhadrosaurs, neoceratopsians, ankylosaurids, pachycephalosaurs, carcharodontosaurines, troodontids, dromaeosaurs and ornithomimosaurs. However, the authors of the paper have suggested that the apparent "new diversification" of dinosaurs during this time is due to sampling biases in the fossil record, and better preserved fossils in Cretaceous age sediments than in earlier Triassic or Jurassic sediments.[2] Genetic evidence indicates a major radiation of phasmatodeans occurred during the KTR, likely in response to a coeval radiation of enantiornitheans and other visual predators.[4] The KTR may have supercharged the contemporary Mesozoic Marine Revolution (MMR) by enhancing weathering and erosion, accelerating the flow of limiting nutrients into the world’s oceans.[5]

A comprehensive molecular study of evolution of mammals at the taxonomic level of family also showed important diversification during the KTR.[6] Similarly, bee pollinator diversification strongly correlates with angiosperm flower appearance and specialization during the same era.[7] Molecular clock analyses of angiosperm evolution suggest that crown group angiosperms may have diverged up to 100 million years before the start of the KTR, although this is possibly due to artefacts of the inabilities of molecular clock estimates to account for explosive accelerations in evolution that may have caused the extremely fast diversification of angiosperms shortly after their first appearance in the fossil record.[8]

For nearly the entirety of Earth's history, including most of the Phanerozoic eon, marine species diversity exceeded terrestrial species diversity, a pattern which was reversed during the Middle Cretaceous as a result of the KTR in what has been termed a biological "great divergence", named after the historical Great Divergence.[9]

## See also

* Cretaceous–Paleogene boundary (K–T boundary)
* Cretaceous–Paleogene extinction event

## References

1. ↑ 1.0 1.1 Benton, Michael James; Wilf, Peter; Sauquet, Hervé (26 October 2021). "The Angiosperm Terrestrial Revolution and the origins of modern biodiversity". New Phytologist 233 (5): 2017–2035. doi:10.1111/nph.17822. PMID 34699613. https://nph.onlinelibrary.wiley.com/doi/10.1111/nph.17822. Retrieved 24 November 2022.
2. ↑ 2.0 2.1 Lloyd, G. T. et al. (2008). "Dinosaurs and the Cretaceous Terrestrial Revolution. 2008". Proceedings of the Royal Society B 275 (1650): 2483–2490. doi:10.1098/rspb.2008.0715. PMID 18647715.
3. ↑ 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. doi:10.1038/s41467-022-32077-7. PMID 35927259.
4. ↑ Tihelka, Erik; Cai, Chenyang; Giacomelli, Mattia; Pisani, Davide; Donoghue, Philip C. J. (11 November 2020). "Integrated phylogenomic and fossil evidence of stick and leaf insects (Phasmatodea) reveal a Permian–Triassic co-origination with insectivores". Royal Society Open Science 7 (11): 201689. doi:10.1098/rsos.201689. PMID 33391817.
5. ↑ Boyce, C. Kevin; Lee, Jung-Eun (1 June 2011). "Could Land Plant Evolution Have Fed the Marine Revolution?" (in en). Paleontological Research 15 (2): 100–105. doi:10.2517/1342-8144-15.2.100. ISSN 1342-8144. http://www.bioone.org/doi/abs/10.2517/1342-8144-15.2.100. Retrieved 29 September 2023.
6. ↑ Meredith, Robert W. (2011). "Impacts of the Cretaceous Terrestrial Revolution and KPg Extinction on Mammal Diversification". Science 334 (6055): 521–524. doi:10.1126/science.1211028. PMID 21940861. Bibcode: 2011Sci...334..521M.
7. ↑ Cardinal, S.; Straka, J.; Danforth, B. N. (2010). "Comprehensive phylogeny of apid bees reveals the evolutionary origins and antiquity of cleptoparasitism". Proceedings of the National Academy of Sciences of the United States of America 107 (37): 16207–11. doi:10.1073/pnas.1006299107. PMID 20805492. Bibcode: 2010PNAS..10716207C.
8. ↑ Barba-Montoya, Jose; Dos Reis, Mario; Schneider, Harald; Donoghue, Philip C. J.; Yang, Ziheng (5 February 2018). "Constraining uncertainty in the timescale of angiosperm evolution and the veracity of a Cretaceous Terrestrial Revolution". New Phytologist 218 (2): 819–834. doi:10.1111/nph.15011. PMID 29399804.
9. ↑ Vermeij, Geerat J.; Grosberg, Richard K. (2 July 2010). "The Great Divergence: When Did Diversity on Land Exceed That in the Sea?". Integrative and Comparative Biology 50 (4): 675–682. doi:10.1093/icb/icq078. PMID 21558232. https://academic.oup.com/icb/article/50/4/675/650584?login=false. Retrieved 1 October 2022.

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