A growing awareness of life in deep igneous crust expands our appreciation for life's distribution in the upper geosphere through time and space, and extends the known inhabitable realm of Earth and possibly beyond. For most of life's history, until plants colonized land in the Ordovician, the deep biosphere was the largest reservoir of living biomass. This suggests that deep crustal habitats played an important role in the evolution and development of the biosphere. Paradoxically, the paleo-perspective of deep life has been largely neglected in the exploration of the deep biosphere as well as in paleontology as a whole. Here, we review the collective understanding of the fossil record in igneous crust with the aim to highlight a rising res...
The discovery of molecular fossils in 2.7-billion-year-old rocks prompted a re-evaluation of microbi...
One of the most profound changes in the history of our planet was the relatively recent emergence of...
A growing literature of deep but also surficial fossilized remains of lithobiological life, often as...
A growing awareness of life in deep igneous crust expands our appreciation for life's distribution i...
The study of life remote in space has strong parallels with the study of life remote in time. Both a...
International audienceLife on the early Earth inhabited a planet whose environment was vastly differ...
The oceanic and continental lithosphere constitutes Earth’s largest microbial habitat, yet it is sca...
International audienceLife on the early Earth inhabited a planet whose environment was vastly differ...
Deep biosphere research is at the scientific frontier of bio- and geo-related sciences, yet it is la...
The rock record provides us with unique evidence for testing models as to when and where cellular li...
The rock record provides us with unique evidence for testing models as to when and where cellular li...
Microfossils, stromatolites, and chemical biosignatures indicate that Earth became a biolog-ical pla...
The landscapes and seascapes of Earth’s surface provide the theatre for life, but to what extent did...
The conventional fossil record is built of hard parts—bones, shells, and decay-resistant organic tis...
Hydrothermal vents are among the most fascinating environments that exist within the modern oceans, ...
The discovery of molecular fossils in 2.7-billion-year-old rocks prompted a re-evaluation of microbi...
One of the most profound changes in the history of our planet was the relatively recent emergence of...
A growing literature of deep but also surficial fossilized remains of lithobiological life, often as...
A growing awareness of life in deep igneous crust expands our appreciation for life's distribution i...
The study of life remote in space has strong parallels with the study of life remote in time. Both a...
International audienceLife on the early Earth inhabited a planet whose environment was vastly differ...
The oceanic and continental lithosphere constitutes Earth’s largest microbial habitat, yet it is sca...
International audienceLife on the early Earth inhabited a planet whose environment was vastly differ...
Deep biosphere research is at the scientific frontier of bio- and geo-related sciences, yet it is la...
The rock record provides us with unique evidence for testing models as to when and where cellular li...
The rock record provides us with unique evidence for testing models as to when and where cellular li...
Microfossils, stromatolites, and chemical biosignatures indicate that Earth became a biolog-ical pla...
The landscapes and seascapes of Earth’s surface provide the theatre for life, but to what extent did...
The conventional fossil record is built of hard parts—bones, shells, and decay-resistant organic tis...
Hydrothermal vents are among the most fascinating environments that exist within the modern oceans, ...
The discovery of molecular fossils in 2.7-billion-year-old rocks prompted a re-evaluation of microbi...
One of the most profound changes in the history of our planet was the relatively recent emergence of...
A growing literature of deep but also surficial fossilized remains of lithobiological life, often as...