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Open Access

Two response patterns to negative environmental changes: Cases from Populus and Metasequoia

Yi ZHANG1,2( )Zhifeng XIONG1Shuangxing GUO3
College of Paleontology, Shenyang Normal University, Shenyang 110034, China
Key Laboratory for Evolution of Past Life in Northeast Asia, Ministry of Natural Resources, Shenyang 110034, China
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
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Abstract

Traditionally, plant distribution is thought to be closely related to environmental factors. But recently, it is found that Populus, quite different from other plant taxa, adapted to negative environmental changes, and successfully migrated to different climate zones from its origin places of warm temperate zone. Conversely, Metasequoia is gradually tending to extinction from the Miocene to Quaternary. Based on above contrary cases, two response patterns of plant to negative environmental changes are proposed. One is active adaptation represented by Populus, the other is passive adaptation represented by Metasequoia. The plants of passive strategy characterized for desert prevention might be easily replaced by those of active strategy characterized for desert utilization. Fast growing plants, such as Populus with characteristics of drought and salt tolerance, wind and sand resistance, are selected in Tarim Basin in southern Xinjiang, China, as a good example of desert utilization in the construction of new highways and towns, not only serve as farmland shelterbelt in sandy area. In addition, Populus with high-altitude and cold adaptation has also been selected as an ideal tree planted in Tibet. Therefore, the idea of using Populus as one of the preferred pioneer trees to colonize Mars is proposed.

References

 
Academia Sinica Silviculturae, Institutum Botabicum, Academiae Sinicae, Collegium Medicinae Pekinense(AIC), et al. 1978. Gymnospermae//Flora Reipublicae Popularis Sinicae: Tomes 7. Beijing: Science Press, 1-542. (in Chinese)
 

An Z S, Zhang P Z, Wang E Q, et al. 2006. Changes of the monsoon-arid environment in China and growth of the Tibetan plateau since the Miocene. Quaternary Sciences, 26: 678-693.

 

Bell W A. 1957. Flora of the Upper Cretaceous Nanaimo Group of Vancouver Island, British Columbia. Geological Survey of Canada, Memoir, 293: 1-84.

 
Boucot A J, Chen X, Scotese C R, et al. 2013. Phanerozoic paleoclimate: An atlas of lithologic indicators of climate. Oklahoma: Society for Sedimentary Geology, 1-478.
 
Deng X C. 2021. Chinese rocket manufacturer outlines manned Mars mission roadmap, timetable. Global Times, 20210623, https://www.globaltimes.cn/page/202106/1226925.shtml.
 

Dickmann I D, Kuzovkina J. 2008. Poplars and willows in the world, with emphasis on silviculturally important species. International Poplar Commission Thematic Papers, 9(2): 1-134.

 

Ding T Y. 1995. Origin, divergence and geographical distribution of Salicaceae. Acta Botanica Yunnanica, 17: 277-290. (in Chinese with English abstract)

 

Eckenwalder J E. 1977. North American cottonwoods(Populus, Salicaceae) of sections Abaso and Aigeiros. Journal of the Arnold Arboretum, 58: 194-208.

 

Fan Y, Zhou M. 2011. Atlas of the world. Beijing: China Map Publishing House, 1-398.

 

Gonzaález-Irusta J M. González-Porto M, Sarralde R, et al. 2015. Comparing species distribution models: A case study of four deep sea urchin species. Hydrobiologia, 745: 43-57.

 

Guo S X. 1975. The plant fossils in Xigaze Group of Mount Qomolngma region. Scientific survey report in Mount Qomalangma region(1966-1968). Paleontology, 1: 411-423.

 
LePage B A, Yang H, Matsumoto M. 2005. The evolution and biogeographic history of Metasequoia//Le Page BA, Christopher W J, Yang H. (Eds.). The geobiology and ecology of Metasequoia. Netherlands: Springer, 3-114.
 

Liu Y J, Arens N C, Li C S. 2007. Range change in Metasequoia: Relationship to palaeoclimate. Botanical Journal of the Linnean Society, 154: 115-127.

 
Li T D. 1995. The uplifting process and mechanism of the Qinhai-Tibet Plateau. Acta Geoscientia Sinica, (1): 1-9.
 

Li J G. 2004. Discovery and preliminary study on palynofossils from the Cenozoic Qiuwu Formation of Xizang(Tibert). Acta Micropalaeontologica Sinica, 21(2): 216-221. (in Chinese with English abstract)

 

Li N. 1995. Studies on the geographic distribution, origin and dispersal of the family Pinaceae Lindl. Acta Phytotaxonormica Sinica, 32(2): 105-130. (in Chinese with English abstract)

 

Manchester R S, Dilcher L D, Tidwell D W. 1986. Interconnected reproductive and vegetative remins of Populus (Salicaceae) from the Middle Eocene Green River Formation, Northeastern Utah. American Journal of Botany, 73: 156-160.

 

Manchester R S, Judd S W, Handley B. 2006. Foliage and fruits of early poplars (Salicaceae: Populus) from the Eocene of Utah, Colorado, and Wyoming. International Journal of Plant Sciences, 167: 897-908.

 

Peel M C, Finlayson B L, Mcmahon T A. 2007. Updated world map of the Köppen-Geiger climate classification. Hydrology and Earth System Sciences Discussions, 4: 439-473.

 

Peppe D J, Hickey L J, Miller l M, et al. 2008. A morphotype catalogue, floristic analysis and stratigraphic description of the aspen shale flora (Cretaceous-Albian) of southwestern Wyoming. Bulletin of the Peabody Museum of Natural History, 49: 181-208.

 

Pritchard H D. 2016. Asia’s glaciers are a regionally important buffer against drought. Nature, 545: 169-174.

 

Rong J Y, Huang B. 2014. Study of mass extinction over the past thirty years: A synopsis. Scientia Sinica Terrae, 44: 377-404.(in Chinese)

 
Scotese C R. 2000. Paleomap project. http://www.scotese.com.
 
Slavov G T, Zhelev P. 2010. Salient biological features, systematics, and genetic variation of Populus//Jansson S, Bhalerao R, Groover A. (Eds.). Genetics and genomics of Populus. New York, Dordrecht, Heidelberg, London: Speinger, 15-38.
 

Sun G, Dilcher D L, Zheng S L, et al. 1998. In search the first flower: A Jurassic angiosperm, Archaefructus, from Northeast China. Nature, 282: 1692-1695.

 

Sutherst R W, Maywald G F. 1985. A computerised system for matching climates in ecology. Agriculture, Ecosystems & Environment, 13: 281-299.

 

Wan X Q, Shi Y J, Huang J L, et al., 2023. An overview and prospect on taxonomy of the genus Populus. Bulletin of Botanical Research, 43(2): 161-168. (In Chinese with English abstract)

 

Wang C, Fang C F. 1984. Flora Reipublicae popularis Sinicae, Tomus 20(2) Salicaceae. Beijing: Science Press, 1-381.

 

Zhou Z B, Xu X W, Lei J Q, et al. 2006. Ecological stability of Tarim Desert Highway shelterbelt. Chinese Science Bulletin, 51(S1): 153-160.

 

Zhang Y, Wang J J. 2015. Historical distribution of Metasequoia referenced to paleoclimate factors. Botanica Pacifica, 4(2): 87-94.

Global Geology
Pages 63-73
Cite this article:
ZHANG Y, XIONG Z, GUO S. Two response patterns to negative environmental changes: Cases from Populus and Metasequoia. Global Geology, 2023, 26(2): 63-73. https://doi.org/10.3969/j.issn.1673-9736.2023.02.01

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Received: 24 August 2022
Accepted: 01 November 2022
Published: 25 May 2023
© 2023 GLOBAL GEOLOGY
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