Finding that limit — the goal of the 62 - day T - Limit campaign, part of the International Ocean Discovery Program — could guide estimates of the abundance and diversity of
ocean floor microbes, which play large roles in biogeochemical cycles.
Not exact matches
But the vents, which are rich in energy sources for
microbes, are poor proxies for most
ocean floor sediments, where scarce nutrients could mean a lower thermal limit.
In deeper parts of the
ocean, the methane released from the
ocean floor would likely never make it up to the atmosphere, since it would get used up by
microbes before it reached the surface.
Samples from a mud volcano contain biological signatures that suggest
microbes lived in the material when it was rock several kilometres beneath the
ocean floor
Many researchers believe iron - metabolizing
microbes might have turned plentiful dissolved iron into minerals, which then settled out of seawater and deposited along the
ocean floor.
Samples from a mud volcano contain biological signatures that suggest
microbes lived in the material when it was several kilometres beneath the
ocean floor.
Field observations of
microbes recovered from deep drill cores, deep mines, and the
ocean floor, coupled with laboratory investigations, reveal that microbial life can exist at conditions of extreme temperatures (to above 110ºC) and pressures (to > 10,000 atmospheres) previous thought impossible.
Over a year ago, scientists uncovered a
microbe that lives in hot - water geysers on the
ocean floor near Iceland.
New keys to understanding the evolution of life on Earth may be found in the
microbes and minerals vented from below the
ocean floor, say scientists at the University of California, Santa Barbara.
Human activities account for 60 percent of methane emissions, but other contributors include plumes from frozen
ocean floors,
microbes, abandoned wells and even beavers of all things.
Jeffrey Marlow, from the Division of Geological and Planetary Sciences at the California Institute of Technology, and colleagues have found that the towering rocks lying at the
ocean floor and near methane seeps, are the dwellings of methane - munching
microbes.
Between 6 and 22 percent of the Earth's methane comes from seeps in the
ocean floor but most of these do not get into the surface nor released into the atmosphere because
microbes consume up to 90 percent of this.