Biogenic-to-lithogenic handoff of particulate Zn affects the Zn cycle in the Southern Ocean.

Zinc (Zn) is vital to marine organisms. Its active uptake by phytoplankton results in a substantial depletion of dissolved Zn, and Zn bound to particulate organic matter replenishes dissolved Zn in the ocean through remineralization. However, we found that particulate Zn changes from Zn bound to phosphoryls in cells to recalcitrant inorganic pools that include biogenic silica, clays, and iron, manganese, and aluminum oxides in the Southern Ocean water column. The abundances of inorganic pools increase with depth and are the only phases preserved in sediments. Changes in the particulate-Zn speciation influence Zn bioavailability and explain the decoupling of Zn and phosphorus and the correlation of Zn and silicon in the water column. These findings reveal a new dimension to the ocean Zn cycle, implicating an underappreciated role of inorganic Zn particles and their impact on biological productivity.

Dissimilatory sulphate reduction in hypersaline coastal pans: an integrated microbiological and geochemical study.

Here, we report on the spatial and temporal variation in sulphate-reducing bacterial community structure and activity in three hypersaline coastal pans. Community structure was determined using denaturing gradient gel electrophoresis (DGGE). Cluster analysis of DGGE patterns indicated that similar microbial populations were generally found in individual pans but varied from one pan to the other. Sulphate reducing bacteria (SRB) were quantified by competitive polymerase chain reaction based on the amplification of the dsrAB genes. Cell numbers and in situ sulphate reduction activities varied between seasons and pans but in general showed low variation in depth. Sulphate reduction activity was not correlated with microbial population size indicating that community composition is relevant for specific microbial processes. Principal component analysis coupled with correlation analyses suggested that salinity, sulphate concentration, C/N ratio and pH were the most important factors in explaining variations in SRB community composition. Most sequences derived from DGGE amplicons belonged to members of the Desulfobacteraceae and Desulfohalobiaceae families.

Chemically and geographically distinct solid-phase iron pools in the Southern Ocean.

Iron is a limiting nutrient in many parts of the oceans, including the unproductive regions of the Southern Ocean. Although the dominant fraction of the marine iron pool occurs in the form of solid-phase particles, its chemical speciation and mineralogy are challenging to characterize on a regional scale. We describe a diverse array of iron particles, ranging from 20 to 700 nanometers in diameter, in the waters of the Southern Ocean euphotic zone. Distinct variations in the oxidation state and composition of these iron particles exist between the coasts of South Africa and Antarctica, with different iron pools occurring in different frontal zones. These speciation variations can result in solubility differences that may affect the production of bioavailable dissolved iron.

Sulphate metabolism among thermophiles and hyperthermophiles in natural aquatic systems.

Although controversial, the idea that hydrothermal systems may have been the site for prebiotic synthesis of organic molecules and origin of life is widely supported. For the nascent life to survive, it must have had some sort of metabolic mechanism for generating energy. However, little is known of the specific metabolic pathways utilized by the early life forms or the effect of high temperatures on their activity. Recent research on natural high temperature aquatic environments, though limited because of difficult field logistics and experimental problems, is revolutionizing our understanding of possible energy-generating redox pathways, such as sulphate reduction. An abridged review of research on thermophilic sulphate reduction is presented here. Because of a complex interplay between microbiological and geochemical entities involved, and the uncertainties that modern hydrothermal systems are proxy for biogeochemical conditions on early Earth, great caution is required for interpretation and extrapolation of data from these studies to primordial times. Furthermore, a general lack of integrated geological and microbiological studies towards a common understanding of origin and sustenance of life on Earth is starkly evident from this review.