168 research outputs found
Novel insights into the Thaumarchaeota in the deepest oceans: their metabolism and potential adaptation mechanisms
Background: Marine Group I (MGI) Thaumarchaeota, which play key roles in the global biogeochemical cycling of nitrogen and carbon (ammonia oxidizers), thrive in the aphotic deep sea with massive populations. Recent studies have revealed that MGI Thaumarchaeota were present in the deepest part of oceans - the hadal zone (depth > 6,000 m, consisting almost entirely of trenches), with the predominant phylotype being distinct from that in the “shallower” deep sea. However, little is known about the metabolism and distribution of these ammonia oxidizers in the hadal water. Results: In this study, metagenomic data were obtained from 0-10,500 m deep seawater samples from the Mariana Trench. The distribution patterns of Thaumarchaeota derived from metagenomics and 16S rRNA gene sequencing were in line with that reported in previous studies: abundance of Thaumarchaeota peaked in bathypelagic zone (depth 1,000 – 4,000 m) and the predominant clade shifted in the hadal zone. Several metagenome-assembled thaumarchaeotal genomes were recovered, including a near-complete one representing the dominant hadal phylotype of MGI. Using comparative genomics we predict that unexpected genes involved in bioenergetics, including two distinct ATP synthase genes (predicted to be coupled with H+ and Na+ respectively), and genes horizontally transferred from other extremophiles, such as those encoding putative di-myo-inositol-phosphate (DIP) synthases, might significantly contribute to the success of this hadal clade under the extreme condition. We also found that hadal MGI have the genetic potential to import a far higher range of organic compounds than their shallower water counterparts. Despite this trait, hadal MDI ammonia oxidation and carbon fixation genes are highly transcribed providing evidence they are likely autotrophic, contributing to the primary production in the aphotic deep sea. Conclusions: Our study reveals potentially novel adaptation mechanisms of deep-sea thaumarchaeotal clades and suggests key functions of deep-sea Thaumarchaeota in carbon and nitrogen cycling
Approximation of singular solutions and singular data for Maxwell’s equations by Lagrange elements
Generation of Optical Chirality Patterns with Plane Waves, Evanescent Waves and Surface Plasmon Waves
We systematically investigate the generation of optical chirality patterns by
applying the superposition of two waves in three scenarios, namely plane waves
in free space, evanescent waves of totally reflected light at dielectric
interface and propagating surface plasmon waves on a metallic surface. In each
scenario, the general analytical solution of the optical chirality pattern is
derived for different polarization states and propagating directions of the two
waves. The analytical solutions are verified by numerical simulations.
Spatially structured optical chirality patterns can be generated in all
scenarios if the incident polarization states and propagation directions are
correctly chosen. Optical chirality enhancement can be obtained from the
constructive interference of free-space circularly polarized light or enhanced
evanescent waves of totally reflected light. Surface plasmon waves do not
provide enhanced optical chirality unless the near-field intensity enhancement
is sufficiently high. The structured optical chirality patterns may find
applications in chirality sorting, chiral imaging and circular dichroism
spectroscopy
Photometric Variability in the CSTAR Field: Results From the 2008 Data Set
The Chinese Small Telescope ARray (CSTAR) is the first telescope facility
built at Dome A, Antarctica. During the 2008 observing season, the installation
provided long-baseline and high-cadence photometric observations in the i-band
for 18,145 targets within 20 deg2 CSTAR field around the South Celestial Pole
for the purpose of monitoring the astronomical observing quality of Dome A and
detecting various types of photometric variability. Using sensitive and robust
detection methods, we discover 274 potential variables from this data set, 83
of which are new discoveries. We characterize most of them, providing the
periods, amplitudes and classes of variability. The catalog of all these
variables is presented along with the discussion of their statistical
properties.Comment: 38 pages, 11 figures, 4 tables; Accepted for publication in ApJ
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