Kinetic modulation of bacterial hydrolases by microbial community structure in coastal waters.

In this study, we hypothesized that shifts in the kinetic parameters of extracellular hydrolytic enzymes may occur as a consequence of seasonal environmental disturbances and would reflect the level of adaptation of the bacterial community to the organic matter of the ecosystem. We measured the activities of enzymes that play a key role in the bacterial growth (leucine aminopeptidase, β- and α-glucosidases) in surface coastal waters of the Eastern Cantabrian Sea and determined their kinetic parameters by computing kinetic models of distinct complexity. Our results revealed the existence of two clearly distinct enzymatic systems operating at different substrate concentrations: a high-affinity system prevailing at low substrate concentrations and a low-affinity system characteristic of high substrate concentrations.

Prokaryotic Capability to Use Organic Substrates Across the Global Tropical and Subtropical Ocean.

Prokaryotes play a fundamental role in decomposing organic matter in the ocean, but little is known about how microbial metabolic capabilities vary at the global ocean scale and what are the drivers causing this variation. We aimed at obtaining the first global exploration of the functional capabilities of prokaryotes in the ocean, with emphasis on the under-sampled meso- and bathypelagic layers. We explored the potential utilization of 95 carbon sources with Biolog GN2 plates in 441 prokaryotic communities sampled from surface to bathypelagic waters (down to 4,000 m) at 111 stations distributed across the tropical and subtropical Atlantic, Indian, and Pacific oceans.

Recurrent seasonal changes in bacterial growth efficiency, metabolism and community composition in coastal waters.

The microbial response to environmental changes in coastal waters of the eastern Cantabrian Sea was explored for four years by analysing a broad set of environmental variables along with bacterial community metabolism and composition. A recurrent seasonal cycle emerged, consisting of two stable periods, characterized by low bacterial metabolic activity (winter) from October to March, and high bacterial metabolic activity (summer) from May to August. These two contrasting periods were linked by short transition periods in April (T ) and September (T ).

Imbalanced nutrient recycling in a warmer ocean driven by differential response of extracellular enzymatic activities.

Ocean oligotrophication concurrent with warming weakens the capacity of marine primary producers to support marine food webs and act as a CO sink, and is believed to result from reduced nutrient inputs associated to the stabilization of the thermocline. However, nutrient supply in the oligotrophic ocean is largely dependent on the recycling of organic matter. This involves hydrolytic processes catalyzed by extracellular enzymes released by bacteria, which temperature dependence has not yet been evaluated.

Changes in bacterial metabolism as a response to dissolved organic matter modification during protozoan grazing in coastal Cantabrian and Mediterranean waters.

We explored how marine dissolved organic matter (DOM) altered by bacterial growth and protozoan grazing modify the metabolism of Southeastern Cantabrian Sea (CS) and NW Mediterranean Sea (MS) coastal bacterial communities. Major metabolic features were measured in treatments with half of the natural water replaced by water with different DOM quality, characterized by fluorescent DOM analysis and collected from key times of the predator-prey curve. In both ecosystems, protozoan-altered DOM led to similar increases in bacterial carbon demand (238% and 213%) and decreases in bacterial growth efficiency (BGE: 56% for the CS and 46% for the MS).

Release and consumption of D-amino acids during growth of marine prokaryotes.

Analysis of the composition of the marine-dissolved organic matter has highlighted the importance of D-amino acids, whose origin is attributed mainly to the remains of bacterial peptidoglycan released as a result of grazing or viral lysis. However, very few studies have focused on the active release of D-amino acids by bacteria. With this purpose, we measured the concentration of dissolved amino acids in both enantiomeric forms with two levels of complexity: axenic cultures of Vibrio furnissii and Vibrio alginolyticus and microcosms created from marine microbial assemblages (Biscay Bay, Cantabrian Sea) with and without heterotrophic nanoflagellates (HNFs).

Chemosensory response of marine flagellate towards L- and D- dissolved free amino acids generated during heavy grazing on bacteria.

This study investigated the generation of dissolved free amino acids (DFAA) by the bacterivorous flagellate Rhynchomonas nasuta when feeding on abundant prey. Specifically, it examined whether this flagellate protist exhibits a chemosensory response towards those amino acids. The concentrations of glycine and the L- and D-enantiomers of glutamate, serine, threonine, alanine, and leucine were determined in co-cultures of the flagellate and bacteria.