TY - JOUR
T1 - Roles of climate niche conservatism and range dynamics in woody plant diversity patterns through the Cenozoic
AU - Shiono, Takayuki
AU - Kusumoto, Buntarou
AU - Yasuhara, Moriaki
AU - Kubota, Yasuhiro
N1 - Funding Information:
We are particularly grateful to palaeontologists, botanical researchers and naturalists in Japan. The palaeontological data compiled in this study were accumulated through the fieldwork of numerous people over many decades. We thank D. Fraser, D. Tittensor, M. Costello and F. Villalobos for discussions and also thank A. J. Kerkhoff and three anonymous referees for constructive comments. Financial support was provided by the Japan Society for the Promotion of Science (no. 15H04424), the Environment Research and Technology Development Fund (4-1501) of the Ministry of the Environment, Japan, Program for Advancing Strategic International Networks to Accelerate the Circulation of Talented Researchers, the Japan Society for the Promotion of Science (to Y.K.), University of the Ryukyus Strategic Research Grant (to B.K.) and Research Grants Council of the Hong Kong Special Administrative Region, China (project codes: HKU 709413P and HKU 17303115; to M.Y.).
Funding Information:
Japan Society for the Promotion of Science, Grant/Award Number: 15H04424; Environment Research and Technology Development Fund, Grant/Award Number: 4-1501; University of the Ryukyus Strategic Research Grant; Research Grants Council of the Hong Kong Special Administrative Region, Grant/Award Number: HKU 709413P and HKU 17303115
Publisher Copyright:
© 2018 John Wiley & Sons Ltd
PY - 2018/7
Y1 - 2018/7
N2 - Aim: Large-scale biodiversity patterns are often discussed in the context of ‘out of the tropics’ (OTT) dynamics and/or tropical niche conservatism (TNC), but empirical evidence of these processes remains very limited. The aim of this study was to infer diversification processes and mechanisms of Cenozoic diversity dynamics using woody angiosperms. Location: East Asian continental islands and global. Time period: Cenozoic. Major taxa studied: Woody plants. Methods: We compiled Cenozoic fossil and modern records for woody angiosperm genera to reconstruct biodiversity patterns. To evaluate the relative importance of TNC and OTT, we investigated extinction/survival patterns and latitudinal range dynamics for each genus, in combination with their clade age (mean family age), cold tolerance and per-genus species richness. Results: We found diversity decreasing with latitude in modern-day flora, but not in the warmer periods of the Neogene and Palaeogene. The percentage of genera surviving decreased with latitude through the Cenozoic. Older genera with less cold tolerance and/or species-poor genera went extinct locally at high latitudes in response to post-Pliocene global cooling. Evolutionarily younger temperate genera dispersed from the extratropics to lower latitudes and the Southern Hemisphere after the Neogene. Main conclusions: The latitudinal diversity gradient (LDG) has rapidly steepened post-Pliocene through: (a) selective extinction in higher latitudes of old, less-diversified tropical genera with low freezing tolerance, and (b) equatorward distributional shift of temperate genera. Both these processes were driven by the high-latitude cooling. Such major roles of TNC and OTT, wherein temperate genera in the Northern Hemisphere expanded through the tropics into higher latitudes of the Southern Hemisphere across climatic boundaries without losing their temperate presence, are in contrast to OTT processes in marine systems. Cenozoic patterns of terrestrial woody angiosperm biodiversity indicate the importance of TNC and high-latitude processes, including the extinction of tropical genera and range contraction or shift of temperate genera.
AB - Aim: Large-scale biodiversity patterns are often discussed in the context of ‘out of the tropics’ (OTT) dynamics and/or tropical niche conservatism (TNC), but empirical evidence of these processes remains very limited. The aim of this study was to infer diversification processes and mechanisms of Cenozoic diversity dynamics using woody angiosperms. Location: East Asian continental islands and global. Time period: Cenozoic. Major taxa studied: Woody plants. Methods: We compiled Cenozoic fossil and modern records for woody angiosperm genera to reconstruct biodiversity patterns. To evaluate the relative importance of TNC and OTT, we investigated extinction/survival patterns and latitudinal range dynamics for each genus, in combination with their clade age (mean family age), cold tolerance and per-genus species richness. Results: We found diversity decreasing with latitude in modern-day flora, but not in the warmer periods of the Neogene and Palaeogene. The percentage of genera surviving decreased with latitude through the Cenozoic. Older genera with less cold tolerance and/or species-poor genera went extinct locally at high latitudes in response to post-Pliocene global cooling. Evolutionarily younger temperate genera dispersed from the extratropics to lower latitudes and the Southern Hemisphere after the Neogene. Main conclusions: The latitudinal diversity gradient (LDG) has rapidly steepened post-Pliocene through: (a) selective extinction in higher latitudes of old, less-diversified tropical genera with low freezing tolerance, and (b) equatorward distributional shift of temperate genera. Both these processes were driven by the high-latitude cooling. Such major roles of TNC and OTT, wherein temperate genera in the Northern Hemisphere expanded through the tropics into higher latitudes of the Southern Hemisphere across climatic boundaries without losing their temperate presence, are in contrast to OTT processes in marine systems. Cenozoic patterns of terrestrial woody angiosperm biodiversity indicate the importance of TNC and high-latitude processes, including the extinction of tropical genera and range contraction or shift of temperate genera.
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U2 - 10.1111/geb.12755
DO - 10.1111/geb.12755
M3 - Article
AN - SCOPUS:85046534988
VL - 27
SP - 865
EP - 874
JO - Global Ecology and Biogeography
JF - Global Ecology and Biogeography
SN - 1466-822X
IS - 7
ER -