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Updated: Jul 28, 2025

Measuring the Structure, Composition, and Change of Underwater Environments with Large-area Imaging
Published on: April 18, 2025
An updated floristic map of the world
Yunpeng Liu1,2, Xiaoting Xu1,3, Dimitar Dimitrov4
1Institute of Ecology, College of Urban and Environmental Sciences, and Key Laboratory of Earth Surface Processes of Ministry of Education, Peking University, 100871, Beijing, China.
This study redefines global floristic realms using plant distributions and phylogeny, revealing plate tectonics as the primary driver of floral evolution and regionalization. Climate plays a minor role in shaping these distinct plant biogeographic regions.
Area of Science:
- Biogeography
- Phylogenetics
- Evolutionary Biology
- Geology
Background:
- Floristic regions organize plant life globally, aiding biological research.
- Existing floristic regions lack evolutionary insights and phylogenetic considerations.
- The roles of tectonic dynamics and climate in shaping floristic regions are unclear.
Purpose of the Study:
- To update global floristic regions by integrating plant distributions and phylogeny.
- To investigate the evolutionary history and temporal changes of floristic regions.
- To determine the influence of tectonic and climatic factors on floristic regionalization.
Main Methods:
- Integrated global distribution data for 12,664 angiosperm genera.
- Incorporated a comprehensive angiosperm phylogeny.
- Analyzed macroevolutionary and paleogeographic processes to define regions.
Main Results:
- Identified eight major floristic realms and 16 nested sub-realms.
- Confirmed Holarctic, Neotropical, and Australian realms; refuted Paleotropical, Antarctic, and Cape realms.
- Found that most realms originated in the Paleogene, primarily shaped by plate tectonics-induced isolation, with minimal climate influence.
Conclusions:
- Integrating phylogenetic and distribution data is crucial for accurate floristic regionalization.
- Plate tectonics is the dominant force in the formation of floristic realms.
- Macroevolutionary and paleogeographic processes significantly shape regional floras over geological time.
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