2009). Generally, subsoils have a high reactive surface area and are less affected by surface agricultural management practices and SOC in deeper soil layers is in the form of organo-mineral complexes, which are important for belowground C stabilization (Rumpel et al. 2015). Understanding these ...
Waters, E. et al. The genome of Nanoarchaeum equitans: insights into early archaeal evolution and derived parasitism. Proc. Natl Acad. Sci. USA 100, 12984–12988 (2003). Article CAS PubMed PubMed Central Google Scholar Casanueva, A. et al. Nanoarchaeal 16S rRNA gene sequences are wide...
Our findings reveal the presence of multiple previously undescribedCa. Thiodiazotropha species found only in lucinids from habitats in deeper waters and/or higher latitudes. A singleCa. Thiodiazotropha species,Ca. T. gloverae, was found in a wide range of both deep sea and temperate shallow-w...
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This can also be applied to the deeper crust-upper mantle, incorporating anisotropy, attenuation, and density-gravity into the model. 4 Summary We present a forward model to quantify the VP, VS, and σ of the solid-liquid mixtures based on previously published experimental and theoretical ...
There is a broad consensus that large-scale pumping of groundwater has altered groundwater dynamics in the Bengal Basin by lowering the water table below large cities and intensively irrigated areas, drawing modern water into deeper aquifers and reversing stream-groundwater exchange during the dry-se...
Clade A4 strains were isolated from For example, Ostreococcus clade A seems to be temperate latitudes, as far North as ~ 49° N or as far typical from surface waters, whereas clade B appears South as ~ 33° S but also from tropical latitudes. The to be associated with deeper layers of...
Gaining a deeper understanding of the contributing factors behind the occurrence of K. brevis HABs could potentially enable us to minimize their impact through the implementation of mitigation strategies and prompt response to stranding events. More effective monitoring strategies may also be developed. ...
compared with the prediction of organic carbon in open oceans, the prediction performance of reefs is relatively poor. The CNN-LSTM model can predict POC in open seas for up to 3 years and CDOM for up to 2 years. The mid-long-term prediction of organic carbon in coral reef waters of ...
At the flowering and boll stage, cotton mainly absorbed soil water from 40–80 cm, which indicates that the roots grow rapidly downward and can absorb the soil water at deeper layers. The contribution ratio of deep soil water to plant water was the largest in the boll opening stage, i.e...