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Abstract
<p id="d5647668e202">Biodiversity is more than the number of species on Earth. It
is also the amount of
unique evolutionary history in the tree of life. We find that losses of this phylogenetic
diversity (PD) are disproportionally large in mammals compared with the number of
species that have recently gone extinct. This lost PD can only be restored with time
as lineages evolve and create new evolutionary history. Without coordinated conservation,
it will likely take millions of years for mammals to naturally recover from the biodiversity
losses they are predicted to endure over the next 50 y. However, by prioritizing PD
in conservation, we could potentially save billions of years of unique evolutionary
history and the important ecological functions they may represent.
</p><p class="first" id="d5647668e205">The incipient sixth mass extinction that started
in the Late Pleistocene has already
erased over 300 mammal species and, with them, more than 2.5 billion y of unique evolutionary
history. At the global scale, this lost phylogenetic diversity (PD) can only be restored
with time as lineages evolve and create new evolutionary history. Given the increasing
rate of extinctions however, can mammals evolve fast enough to recover their lost
PD on a human time scale? We use a birth–death tree framework to show that even if
extinction rates slow to preanthropogenic background levels, recovery of lost PD will
likely take millions of years. These findings emphasize the severity of the potential
sixth mass extinction and the need to avoid the loss of unique evolutionary history
now.
</p>
Large herbivores and carnivores (the megafauna) have been in a state of decline and extinction since the Late Pleistocene, both on land and more recently in the oceans. Much has been written on the timing and causes of these declines, but only recently has scientific attention focused on the consequences of these declines for ecosystem function. Here, we review progress in our understanding of how megafauna affect ecosystem physical and trophic structure, species composition, biogeochemistry, and climate, drawing on special features of PNAS and Ecography that have been published as a result of an international workshop on this topic held in Oxford in 2014. Insights emerging from this work have consequences for our understanding of changes in biosphere function since the Late Pleistocene and of the functioning of contemporary ecosystems, as well as offering a rationale and framework for scientifically informed restoration of megafaunal function where possible and appropriate.
The extinction of dinosaurs at the Cretaceous/Paleogene (K/Pg) boundary was the seminal event that opened the door for the subsequent diversification of terrestrial mammals. Our compilation of maximum body size at the ordinal level by sub-epoch shows a near-exponential increase after the K/Pg. On each continent, the maximum size of mammals leveled off after 40 million years ago and thereafter remained approximately constant. There was remarkable congruence in the rate, trajectory, and upper limit across continents, orders, and trophic guilds, despite differences in geological and climatic history, turnover of lineages, and ecological variation. Our analysis suggests that although the primary driver for the evolution of giant mammals was diversification to fill ecological niches, environmental temperature and land area may have ultimately constrained the maximum size achieved.
The most rapid species radiations have been reported from 'evolutionary laboratories', such as the Andes and the Cape of South Africa, leading to the prevailing view that diversification elsewhere has not been as dramatic. However, few studies have explicitly assessed rates of diversification in northern regions such as Europe. Here, we show that carnations (Dianthus, Caryophyllaceae), a well-known group of plants from temperate Eurasia, have diversified at the most rapid rate ever reported in plants or terrestrial vertebrates. Using phylogenetic methods, we found that the majority of species of carnations belong to a lineage that is remarkably species-rich in Europe, and arose at the rate of 2.2-7.6 species per million years. Unlike most previous studies that have inferred rates of diversification in young diverse groups, we use a conservative approach throughout that explicitly incorporates the uncertainties associated with phylogenetic inference, molecular dating and incomplete taxon sampling. We detected a shift in diversification rates of carnations coinciding with a period of increase in climatic aridity in the Pleistocene, suggesting a link between climate and biodiversity. This explosive radiation suggests that Europe, the continent with the world's best-studied flora, has been underestimated as a cradle of recent and rapid speciation.
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