History of life

Summary

The history of life on Earth traces the processes by which living and fossil organisms evolved, from the earliest emergence of life to present day. Earth formed about 4.5 billion years ago (abbreviated as Ga, for gigaannum) and evidence suggests that life emerged prior to 3.7 Ga. Although there is some evidence of life as early as 4.1 to 4.28 Ga, it remains controversial due to the possible non-biological formation of the purported fossils. The similarities among all known present-day species indicate that they have diverged through the process of evolution from a common ancestor. Only a very small percentage of species have been identified: one estimate claims that Earth may have 1 trillion species. However, only 1.75–1.8 million have been named and 1.8 million documented in a central database. These currently living species represent less than one percent of all species that have ever lived on Earth. The earliest evidence of life comes from biogenic carbon signatures and stromatolite fossils discovered in 3.7 billion-year-old metasedimentary rocks from western Greenland. In 2015, possible "remains of biotic life" were found in 4.1 billion-year-old rocks in Western Australia. In March 2017, putative evidence of possibly the oldest forms of life on Earth was reported in the form of fossilized microorganisms discovered in hydrothermal vent precipitates in the Nuvvuagittuq Belt of Quebec, Canada, that may have lived as early as 4.28 billion years ago, not long after the oceans formed 4.4 billion years ago, and not long after the formation of the Earth 4.54 billion years ago. Microbial mats of coexisting bacteria and archaea were the dominant form of life in the early Archean eon and many of the major steps in early evolution are thought to have taken place in this environment. The evolution of photosynthesis by cyanobacteria, around 3.5 Ga, eventually led to a buildup of its waste product, oxygen, in the ocean and then the atmosphere after depleting all available reductant substances on the Earth's surface, leading to the Great Oxygenation Event, beginning around 2.

Official source

https://en.wikipedia.org/wiki/History_of_life

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Genetic variation and evolutionary history of a mycorrhizal fungus regulate the currency of exchange in symbiosis with the food security crop cassava

Romain Savary, Cindy Dupuis

Most land plants form symbioses with arbuscular mycorrhizal fungi (AMF). Diversity of AMF increases plant community productivity and plant diversity. For decades, it was known that plants trade carbohydrates for phosphate with their fungal symbionts. However, recent studies show that plant-derived lipids probably represent the most essential currency of exchange. Understanding the regulation of plant genes involved in the currency of exchange is crucial to understanding stability of this mutualism. Plants encounter many different AMF genotypes that vary greatly in the benefit they confer to plants. Yet the role that fungal genetic variation plays in the regulation of this currency has not received much attention. We used a high-resolution phylogeny of one AMF species (Rhizophagus irregularis) to show that fungal genetic variation drives the regulation of the plant fatty acid pathway in cassava (Manihot esculenta); a pathway regulating one of the essential currencies of trade in the symbiosis. The regulation of this pathway was explained by clearly defined patterns of fungal genome-wide variation representing the precise fungal evolutionary history. This represents the first demonstrated link between the genetics of AMF and reprogramming of an essential plant pathway regulating the currency of exchange in the symbiosis. The transcription factor RAM1 was also revealed as the dominant gene in the fatty acid plant gene co-expression network. Our study highlights the crucial role of variation in fungal genomes in the trade of resources in this important symbiosis and also opens the door to discovering characteristics of AMF genomes responsible for interactions between AMF and cassava that will lead to optimal cassava growth.

2020

Transposable elements (TEs) are genetic units capable of spreading within the genomes of their host. TEs contribute a readily recognizable 45% of the human DNA, reflecting in part their co-option for some as source of protein-coding sequences, for others as regulators of genome architecture and expression. Nevertheless, new TE integrants can occasionally cause diseases. The KZFP/KAP1 (KRAB-Zinc Finger Protein /KRAB-associated Protein 1) system plays a major role in the transcriptional control of TEs. Encoded in the hundreds by the genomes of most higher vertebrates, KZFPs are endowed with a N-terminal KRAB (KruÌppel- associated box) domain, some of which can recruit KAP1, and a C-terminal array of zinc fingers (ZNF) with polynucleotide binding potential. When we started this work, KZFP genes were thought to be restricted to tetrapods, and a few of their products had been found to tether KAP1 and associated heterochromatin-inducing factors to TE-derived sequences during mouse or human early embryogenesis, resulting in the deposition at these loci of H3K9me3 (histone 3 trimethylated on lysine 9) and DNA methylation, two repressive marks. Additionally, the KZFP/KAP1 system had been implicated in events as diverse as imprinting, cell differentiation and metabolic homeostasis. In order to gain insight into the biology of human KZFPs, we first performed a large-scale identification of their genomic targets. We found that the majority was enriched at TEs, where they bound to regions also recognized by other TFs. Accordingly, many KZFP-targeted TE loci displayed differential chromatin patterns in human tissues, consistent notably with their putative role of cell-specific enhancers. This strongly suggests that KZFPs participate in orchestrating TE-modulated regulatory networks. Finally, we could trace KZFP genes to a common ancestor of the coelacanth, lungfishes and tetrapods, and determined that their evolutionary emergence was most often contemporaneous to that of their TE targets, with signs supporting both an arms race and a domestication model. To pursue this exploration, we analyzed the protein partners of more than a hundred human KZFPs. We could observe that the interactome of evolutionarily recent KZFPs mainly comprised KAP1 and associated effectors, whereas that of more ancient family members, conserved from marsupials to sauropsids, tended not to associate with KAP1 and were likely to engage in interactions with more original factors, including proteins related to RNA processing or genome architecture. While these results suggested that KAP1 binding might have been a late emerging property of KZFPs, we could demonstrate that KRAB domains derived from Latimeria chalumnae associated with the cognate KAP1 protein, albeit not with its human orthologue. These results support a model whereby KZFPs first emerged as TE- controlling repressors, were continuously renewed by turnover of their hostsâ TE loads, and occasionally produced derivatives that escaped this evolutionary flushing by development and exaptation of novel functions. In sum, this work provides important insights into the evolutionary history and biological function of KRAB zinc finger proteins, the largest family of transcriptional regulators encoded by human and other higher vertebrates.

EPFL2019

Genetic consequences of population expansions and contractions in the common hippopotamus (Hippopotamus amphibius) since the Late Pleistocene

Séverine Vuilleumier Varisco, Pierre Joly

Over the past two decades, an increasing amount of phylogeographic work has substantially improved our understanding of African biogeography, in particular the role played by Pleistocene pluvial-drought cycles on terrestrial vertebrates. However, still little is known on the evolutionary history of semi-aquatic animals, which faced tremendous challenges imposed by unpredictable availability of water resources. In this study, we investigate the Late Pleistocene history of the common hippopotamus (Hippopotamus amphibius), using mitochondrial and nuclear DNA sequence variation and range-wide sampling. We documented a global demographic and spatial expansion approximately 0.1-0.3Myr ago, most likely associated with an episode of massive drainage overflow. These events presumably enabled a historical continent-wide gene flow among hippopotamus populations, and hence, no clear continental-scale genetic structuring remains. Nevertheless, present-day hippopotamus populations are genetically disconnected, probably as a result of the mid-Holocene aridification and contemporary anthropogenic pressures. This unique pattern contrasts with the biogeographic paradigms established for savannah-adapted ungulate mammals and should be further investigated in other water-associated taxa. Our study has important consequences for the conservation of the hippo, an emblematic but threatened species that requires specific protection to curtail its long-term decline

Wiley-Blackwell2015

EPFL2019