scholarly journals Five Metagenome-Assembled Genomes of the Rare Phylum CSSED10-310 from Zodletone Spring (Oklahoma, USA)

2021 ◽  
Vol 10 (26) ◽  
Author(s):  
Archana Yadav ◽  
C. Ryan Hahn ◽  
Mostafa S. Elshahed ◽  
Noha H. Youssef
Keyword(s):  

We analyzed five metagenome-assembled genomes (MAGs) belonging to the rare, yet-uncultured phylum CSSED10-310 recovered from the anoxic sediments of Zodletone Spring (Oklahoma, USA). Our analysis suggests their potential involvement in sulfite respiration.

2011 ◽  
Vol 40 (2) ◽  
pp. 484-491 ◽  
Author(s):  
Heather J. Shipley ◽  
Yan Gao ◽  
Amy T. Kan ◽  
Mason B. Tomson

2017 ◽  
Vol 51 (19) ◽  
pp. 11039-11047 ◽  
Author(s):  
Sharon E. Bone ◽  
Melanie R. Cahill ◽  
Morris E. Jones ◽  
Scott Fendorf ◽  
James Davis ◽  
...  

2015 ◽  
Vol 282 (1817) ◽  
pp. 20152025 ◽  
Author(s):  
Elias Broman ◽  
Martin Brüsin ◽  
Mark Dopson ◽  
Samuel Hylander

Many coastal marine systems have extensive areas with anoxic sediments and it is not well known how these conditions affect the benthic–pelagic coupling. Zooplankton lay their eggs in the pelagic zone, and some sink and lie dormant in the sediment, before hatched zooplankton return to the water column. In this study, we investigated how oxygenation of long-term anoxic sediments affects the hatching frequency of dormant zooplankton eggs. Anoxic sediments from the brackish Baltic Sea were sampled and incubated for 26 days with constant aeration whereby, the sediment surface and the overlying water were turned oxic. Newly hatched rotifers and copepod nauplii (juveniles) were observed after 5 and 8 days, respectively. Approximately 1.5 × 10 5 nauplii m −2 emerged from sediment turned oxic compared with 0.02 × 10 5 m −2 from controls maintained anoxic. This study demonstrated that re-oxygenation of anoxic sediments activated a large pool of buried zooplankton eggs, strengthening the benthic–pelagic coupling of the system. Modelling of the studied anoxic zone suggested that a substantial part of the pelagic copepod population can derive from hatching of dormant eggs. We suggest that this process should be included in future studies to understand population dynamics and carbon flows in marine pelagic systems.


Author(s):  
Carolina Reyes ◽  
Jonathan R. Lloyd ◽  
Chad W. Saltikov
Keyword(s):  

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