Angiosperms are the most diverse and abundant plant taxon today and dominate the majority of Earth's terrestrial ecosystems. They underwent rapid divergence and biogeographic expansion from the early to the middle Cretaceous. Yet, transformative ecosystem change brought about by the increased ecological dominance of angiosperms unfolded progressively until the Late Cretaceous. After the Cretaceous–Paleogene (K–Pg) boundary, angiosperms restructured terrestrial ecosystems towards a modern form. By the Neogene, crown groups that make up modern terrestrial angiosperm biodiversity radiated, and regional floristic distinctions were established concurrently with the steepened latitudinal and vertical temperature gradients. Here, we summarize, based on fossils and molecular evidence, when and how angiosperms came to diversify, dominate, and shape terrestrial ecosystems, leading to the emergence and spread of angiosperm-dominated floras. We highlight five major phases of angiosperm evolution that took place against a background of palaeogeography and climate changes. There is a consistent delay in ecological dominance after lineage origination and taxonomic diversification, as a result of which angiosperms did not achieve ecological dominance across terrestrial biomes in a single step. The patterns of diversity seen among extant angiosperms, the dominant angiosperm groups within modern ecosystems, and the restriction of different groups of angiosperms to different parts of the world, reflect the contingent nature of the process of lineage diversification in the context of long-term, substantial and ongoing environmental change. Determining the origins, diversification, and ecological dominance of angiosperms continues to be a challenge and requires elucidation of their early forms, functions, habitats, and environmental interactions throughout evolutionary history.
{"title":"The stepwise rise of angiosperm-dominated terrestrial ecosystems","authors":"Wenna Ding, Daniele Silvestro, Renske E. Onstein, Mengxiao Wu, Zhekun Zhou, Yaowu Xing","doi":"10.1111/brv.70039","DOIUrl":"10.1111/brv.70039","url":null,"abstract":"<p>Angiosperms are the most diverse and abundant plant taxon today and dominate the majority of Earth's terrestrial ecosystems. They underwent rapid divergence and biogeographic expansion from the early to the middle Cretaceous. Yet, transformative ecosystem change brought about by the increased ecological dominance of angiosperms unfolded progressively until the Late Cretaceous. After the Cretaceous–Paleogene (K–Pg) boundary, angiosperms restructured terrestrial ecosystems towards a modern form. By the Neogene, crown groups that make up modern terrestrial angiosperm biodiversity radiated, and regional floristic distinctions were established concurrently with the steepened latitudinal and vertical temperature gradients. Here, we summarize, based on fossils and molecular evidence, when and how angiosperms came to diversify, dominate, and shape terrestrial ecosystems, leading to the emergence and spread of angiosperm-dominated floras. We highlight five major phases of angiosperm evolution that took place against a background of palaeogeography and climate changes. There is a consistent delay in ecological dominance after lineage origination and taxonomic diversification, as a result of which angiosperms did not achieve ecological dominance across terrestrial biomes in a single step. The patterns of diversity seen among extant angiosperms, the dominant angiosperm groups within modern ecosystems, and the restriction of different groups of angiosperms to different parts of the world, reflect the contingent nature of the process of lineage diversification in the context of long-term, substantial and ongoing environmental change. Determining the origins, diversification, and ecological dominance of angiosperms continues to be a challenge and requires elucidation of their early forms, functions, habitats, and environmental interactions throughout evolutionary history.</p>","PeriodicalId":133,"journal":{"name":"Biological Reviews","volume":"100 5","pages":"2131-2149"},"PeriodicalIF":11.7,"publicationDate":"2025-05-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/brv.70039","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144179731","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"生物学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
The mechanisms of fern dispersal are under-studied and there are few data to support the vectors assumed to drive patterns of sporophyte occurrence and speciation. Although wind is generally the fern spore dispersal vector described in the literature, there has always been competing evidence supporting alternate vectors. Despite this, established patterns of dispersal are generally discussed in the context of wind. The assumptions around wind as a dispersal vector and the possibilities of single-spore establishment have confounded discussions on effective dispersal of fern spore, fern meta-population dynamics, and fern speciation. In this study, I review (i) the importance of spore load across taxa, (ii) evidence for vectors of fern spore, (iii) the environmental tolerances of fern life stages, and (iv) the relevance of, and constraints on, different dispersal vectors in the context of increasingly hazardous landscape matrices. I conclude that whilst wind is an important dispersal vector in non-hazardous landscapes, directed dispersal by an animal vector to isolated safe sites in a hazardous landscape matrix may be key for fern metapopulations and communities.
{"title":"Effective dispersal of fern spore and the ecological relevance of zoochory","authors":"James M. R. Brock","doi":"10.1111/brv.70038","DOIUrl":"10.1111/brv.70038","url":null,"abstract":"<p>The mechanisms of fern dispersal are under-studied and there are few data to support the vectors assumed to drive patterns of sporophyte occurrence and speciation. Although wind is generally the fern spore dispersal vector described in the literature, there has always been competing evidence supporting alternate vectors. Despite this, established patterns of dispersal are generally discussed in the context of wind. The assumptions around wind as a dispersal vector and the possibilities of single-spore establishment have confounded discussions on effective dispersal of fern spore, fern meta-population dynamics, and fern speciation. In this study, I review (<i>i</i>) the importance of spore load across taxa, (<i>ii</i>) evidence for vectors of fern spore, (<i>iii</i>) the environmental tolerances of fern life stages, and (<i>iv</i>) the relevance of, and constraints on, different dispersal vectors in the context of increasingly hazardous landscape matrices. I conclude that whilst wind is an important dispersal vector in non-hazardous landscapes, directed dispersal by an animal vector to isolated safe sites in a hazardous landscape matrix may be key for fern metapopulations and communities.</p>","PeriodicalId":133,"journal":{"name":"Biological Reviews","volume":"100 5","pages":"2116-2130"},"PeriodicalIF":11.7,"publicationDate":"2025-05-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/brv.70038","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144172243","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"生物学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}