A ravenous predator also survives in these hellish conditions: a roundworm that researchers describe today as the first multicellular organism to be found in
the deep subsurface of Earth.
Nematoda from the terrestrial
deep subsurface of South Africa.
Not exact matches
Yet a
deep hole discovered on the moon could one day be the entrance to a
subsurface base that would keep colonists safe from the ravages
of space.
Data from a 1970s international research effort to explore the
subsurface of the region, called the Dry Valleys Drilling Project, found tantalizing geophysical evidence — seismic and electrical resistivity data — that hinted at liquid water
deep below.
Although geologists can use seismic data from large earthquakes to see features
deep in the earth, the shallow
subsurface geology
of the park has remained a mystery, because mapping it out would require capturing everyday miniature ground movement and seismic energy on a much smaller scale.
Lothar Stramma, a physical oceanographer at the Christian Albrechts University
of Kiel in Germany and his associates describe the hypoxic problem as global in a paper accepted for publication in
Deep - Sea Research, stating that tropical low - oxygen zones have expanded horizontally and vertically around the world, and that
subsurface oxygen has decreased adjacent to most continental shelves.
Even as phytoplankton blooms sequester new carbon, the upwelling
of deep,
subsurface water currents in the region bring old, once - sequestered carbon back to the surface waters, allowing for exchange with the atmosphere.
The potential exploration
of other
deep sea or
subsurface ecosystems will raise other «Schrödinger's cat» dilemmas.
Among other things, GRACE may have found a crater
deep under the Antarctic ice that may mark an asteroid impact greater than the one that doomed the dinosaurs, measured the seafloor displacement that triggered the tsunami
of 2004, and quantified changes in
subsurface water in the Amazon and Congo river basins.
With his ground - penetrating radar, Michele Pipan, a geophysicist at the University
of Trieste, gradually mapped the
subsurface structures (some three to four meters
deep) below the 500 - meter shore perimeter.
«We probably would approach the future
of Mars exploration — particularly accessing habitable zones
of liquid water in the
deep subsurface — more cautiously, because life could still be there.
Meanwhile, the lander will keep digging and analyzing
deeper — toward the
subsurface ice reported last week (ScienceNOW, 20 June), in search
of water's history on Mars.
The
subsurface oceans that are believed to exist on Europa and Enceladus, would have conditions similar to the
deep oceans
of Earth where tardigrades are found, volcanic vents providing heat in an environment devoid
of light.
Quantifying the global hydrogen budget is key to understanding the amount
of Earth's biomass that is in the
subsurface, as many
deep ecosystems contain chemolithotrophic — so - called «rock - eating» — organisms that consume hydrogen.
The most popular explanations today are that it was either born as an inflating half dome
of magma squeezed in between
subsurface layers
of rock or within a conduit
deep inside a volcano.
Pluto is thought to possess a
subsurface ocean, which is not so much a sign
of water as it is a tremendous clue that other dwarf planets in
deep space also may contain similarly exotic oceans, naturally leading to the question
of life, said one co-investigator with NASA's New Horizon mission to Pluto and the Kuiper Belt.
Conditions in its
subsurface global water ocean are thought to be similar to those
deep in Earth's oceans, where a wide variety
of life thrives.
The science
of Deep Earth Imaging will help us more precisely image
subsurface rock properties to unlock the potential
of this vast and relatively under - explored area.
No one knows the origin
of this ice, but one possibility is that ice - rich bodies, such as comets, left part
of their ice
deep in the
subsurface following impact.
We're developing
Deep Earth Imaging technology to allow geologists to create precise images
of subsurface rock properties, as if the regolith material is transparent.
The
Deep Earth Imaging Future Science Platform aims to more precisely and more accurately image the
subsurface and understand its geophysical and geochemical properties, unlocking the resource potential
of a vast, under - explored part
of Australia.
Once ignited, these fires are particularly difficult to extinguish despite extensive rains, weather changes or firefighting attempts, and can persist for long periods
of time (months, years), spreading
deep (5 meters) and over extensive areas
of forest
subsurface.
Yan, X-H., H. Su, and W. Zhang, 2014: Contribution
of global
subsurface and
deeper ocean warming to recent global surface warming hiatus.
The improved simulation
of ENSO amplitude is mainly due to the reasonable representation
of the thermocline and thermodynamic feedbacks: On the one hand, the
deeper mean thermocline results in a weakened thermocline response to the zonal wind stress anomaly, and the looser vertical stratification
of mean temperature leads to a weakened response
of anomalous
subsurface temperature to anomalous thermocline depth, both
of which cause the reduced thermocline feedback in g2; on the other hand, the alleviated cold bias
of mean sea surface temperature leads to more reasonable thermodynamic feedback in g2.
This suggests that the Tambora
subsurface temperature and sea level perturbations could last well into the 20th century, interfering with the effects
of the devastating Krakatau, Santa Maria, and Katmai eruptions which occurred respectively in 1883, 1902, and 1912, producing a cumulative impact on the
deep ocean thermal structure in the 20th century.
dana1981 - An additional part
of that correction is that the
deeper subsurface Antarctic waters are (relatively) warmer than surface waters, not colder as stated in the OP.
This includes maintaining Argo, the main system for monitoring ocean heat content, and the development
of Deep Argo to monitor the lower half of the ocean; the use of ship - based subsurface ocean temperature monitoring programs; advancements in robotic technologies such as autonomous underwater vehicles to monitor waters adjacent to land (like islands or coastal regions); and further development of real - or near - real - time deep ocean remote sensing meth
Deep Argo to monitor the lower half
of the ocean; the use
of ship - based
subsurface ocean temperature monitoring programs; advancements in robotic technologies such as autonomous underwater vehicles to monitor waters adjacent to land (like islands or coastal regions); and further development
of real - or near - real - time
deep ocean remote sensing meth
deep ocean remote sensing methods.
Another big outcome is a
deeper understanding
of the roles
subsurface microbes play in globally important carbon, hydrogen, nitrogen, and sulfur cycles.
And in fact, recent observational (Lavender et al., 2000; Fischer and Schott, 2002; Bower et al., 2009) and modeling studies (Gary et al., 2011; Lozier et al., 2010)
of subsurface floats have revealed that the DWBC is not the sole, and perhaps not even the dominant, conduit for the transport
of the waters within the
deep limb
of the AMOC.
While such models lack adequate observational datasets
of subsurface soil properties and / or geology, it is clear that the time scale for
deep permafrost thaw is measured in centuries, not years.