Related Experiment Video
Updated: Jan 31, 2026

A Novel Bioreactor for High Density Cultivation of Diverse Microbial Communities
Published on: December 25, 2015
Microbial community composition and diversity in the Indian Ocean deep sea REY-rich muds
Shuyan Wang1,2,3, Miao Yu4, Jiaqiang Wei1,2,3
1Key Lab of Marine Bioactive Substances of SOA, The First Institute of Oceanography, Qingdao, China.
Abstract:
Studies about the composition and diversity of microbial community in the Rare Earth Elements-rich muds are limited. In this research, we conducted a characterization for the composition and diversity of bacterial and archaeal communities from rare earth elements-rich gravity core sediment at approximately 4800 meters deep in the Indian Ocean by Illumina high-throughput sequencing targeting 16S rRNA genes. The results showed that the most abundant bacteria were Proteobacteria, followed by Firmicutes and Actinobacteria. Amongst Proteobacteria, Gammaproteobacteria are present in all sections of this sediment core accounted for a particularly large proportion of bacterial sequences. Candidatus Nitrosopumilus, with a higher relative abundance in our samples, belongs to Thaumarchaeota. This is the first report on the composition and diversity of rare earth elements-rich muds microbial communities in the Indian Ocean deep sea.
Related Concept Videos
Gene Regulation in Microbial Communities: Quorum Sensing
What are Populations and Communities?
Keystone Species
Classifying Matter by Composition
According to its composition, the matter can be classified into two broad categories — pure substances and mixtures.
A pure substance is a form of matter that has a constant composition throughout with uniform properties. For example, any sample of sucrose has the same composition and same physical properties, such as melting point, color, and sweetness, regardless of the source from which it is isolated.
A mixture is composed of two or...
Effect of Sea Water on Concrete
Concrete in areas between tide marks,...
Diversity of Archaea I

