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Evolution of Grasses and Grassland Ecosystems

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TLDR
The evolution and subsequent ecological expansion of grasses (Poaceae) since the Late Cretaceous have resulted in the establishment of one of Earth's dominant biomes, the temperate and tropical grasslands, at the expense of forests as mentioned in this paper.
Abstract
The evolution and subsequent ecological expansion of grasses (Poaceae) since the Late Cretaceous have resulted in the establishment of one of Earth’s dominant biomes, the temperate and tropical grasslands, at the expense of forests. In the past decades, several new approaches have been applied to the fossil record of grasses to elucidate the patterns and processes of this ecosystem transformation. The data indicate that the development of grassland ecosystems on most continents was a multistage process involving the Paleogene appearance of (C3 and C4) open-habitat grasses, the mid-late Cenozoic spread of C3 grass-dominated habitats, and, finally, the Late Neogene expansion of C4 grasses at tropical-subtropical latitudes. The evolution of herbivores adapted to grasslands did not necessarily coincide with the spread of open-habitat grasses. In addition, the timing of these evolutionary and ecological events varied between regions. Consequently, region-by-region investigations using both direct (plant fossils) and indirect (e.g., stable carbon isotopes, faunas) evidence are required for a full understanding of the tempo and mode of grass and grassland evolution.

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Ancient hybridizations among the ancestral genomes of bread wheat

TL;DR: It is implied that the present-day bread wheat genome is a product of multiple rounds of hybrid speciation (homoploid and polyploid) and lay the foundation for a new framework for understanding the wheat genome as a multilevel phylogenetic mosaic.
Journal ArticleDOI

Photorespiration and the Evolution of C4 Photosynthesis

TL;DR: Phylogenetically informed research indicates that the repositioning of mitochondria in the bundle sheath is one of the earliest steps in C(4) evolution, as it may establish a single-celled mechanism to scavenge photorespired CO(2) produced in the bundles sheath cells.
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Late Miocene global cooling and the rise of modern ecosystems

TL;DR: A period of continental aridification and ecosystem change occurred about seven million years ago and a global sea surface temperature reconstruction identifies cooling temperatures and a strengthened meridional temperature gradient at this time.
Journal ArticleDOI

The sheep genome illuminates biology of the rumen and lipid metabolism

Yu Jiang, +79 more
- 06 Jun 2014 - 
TL;DR: A genome for ewe and ewe Sheep-specific genetic changes underlie differences in lipid metabolism between sheep and other mammals, and may have contributed to the production of wool.
References
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Journal ArticleDOI

Global vegetation change through the Miocene/Pliocene boundary

TL;DR: For example, this paper found that between 8 and 6 million years ago, there was a global increase in the biomass of plants using C4 photosynthesis as indicated by changes in the carbon isotope ratios of fossil tooth enamel in Asia, Africa, North America and South America.
Book

Phytoliths: A Comprehensive Guide for Archaeologists and Paleoecologists

TL;DR: The production, deposition, and dissolution of phytoliths have been extensively studied in the field of bioarchaeology as discussed by the authors, including the role of these artifacts in archaeological reconstruction.
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The evolution of C4 photosynthesis

TL;DR: Gene duplication followed by neo- and nonfunctionalization are the leading mechanisms for creating C4 genomes, with selection for carbon conservation traits under conditions promoting high photorespiration being the ultimate factor behind the origin of C4 photosynthesis.
Journal ArticleDOI

What Limits Trees in C4 Grasslands and Savannas

TL;DR: The extent of this climate mismatch has been revealed by physiologically based global vegetation simulations and by large empirical data sets, and the implication is that ecosystem structure and function depend on demographic transitions.
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Trending Questions (1)
How did the expansion of grasslands?

The expansion of grasslands occurred through a multistage process involving the appearance of open-habitat grasses in the Paleogene, spread of C3 grass-dominated habitats, and later expansion of C4 grasses.