The symbiotic role of marine microbes on living surfaces

Every surface immersed in the sea rapidly becomes covered with a biofilm. On inanimate surfaces, this is often followed by colonisation by larger organisms, and general macrofouling. On the other hand, the majority of marine organisms remain relatively free from macrofouling, although some may be covered in a thin film of epibiotic bacteria. The role of these bacteria in maintaining the health of the host has received little attention. Here we describe an ecological role for epibiotic bacteria from seaweed surfaces. These epibionts may play a protective role, releasing compounds into the surrounding seawater that help prevent extensive fouling of the surface. These compounds may also have industrial and medical applications. The relative ease of culturing these microbes, compared to other bacteria that produce active compounds suggests seaweed-associated bacteria may be useful in bioprocess applications, such as the production of antimicrobial or antifouling compounds.     

The expanding role of marine microbes in pharmaceutical development

Marine microbes have received growing attention as sources of bioactive metabolites and offer a unique opportunity to both increase the number of marine natural products in clinical trials as well as expedite their development. This review focuses specifically on those molecules currently in the clinical pipeline that are established or highly likely to be produced by bacteria based on expanding circumstantial evidence. We also include an example of how compounds from harmful algal blooms may yield both tools for measuring environmental change as well as leads for pharmaceutical development. An example of the karlotoxin class of compounds isolated from the dinoflagellate Karlodinium veneficum reveals a significant environmental impact in the form of massive fish kills, but also provides opportunities to construct new molecules for the control of cancer and serum cholesterol assisted by tools associated with rational drug design.     

Prochlorococcus, a marine photosynthetic prokaryote of global significance.

The minute photosynthetic prokaryote Prochlorococcus, which was discovered about 10 years ago, has proven exceptional from several standpoints. Its tiny size (0.5 to 0.7 microm in diameter) makes it the smallest known photosynthetic organism. Its ubiquity within the 40 degrees S to 40 degrees N latitudinal band of oceans and its occurrence at high density from the surface down to depths of 200 m make it presumably the most abundant photosynthetic organism on Earth. Prochlorococcus typically divides once a day in the subsurface layer of oligotrophic areas, where it dominates the photosynthetic biomass. It also possesses a remarkable pigment complement which includes divinyl derivatives of chlorophyll a (Chl a) and Chl b, the so-called Chl a2 and Chl b2, and, in some strains, small amounts of a new type of phycoerythrin. Phylogenetically, Prochlorococcus has also proven fascinating. Recent studies suggest that it evolved from an ancestral cyanobacterium by reducing its cell and genome sizes and by recruiting a protein originally synthesized under conditions of iron depletion to build a reduced antenna system as a replacement for large phycobilisomes. Environmental constraints clearly played a predominant role in Prochlorococcus evolution. Its tiny size is an advantage for its adaptation to nutrient-deprived environments. Furthermore, genetically distinct ecotypes, with different antenna systems and ecophysiological characteristics, are present at depth and in surface waters. This vertical species variation has allowed Prochlorococcus to adapt to the natural light gradient occurring in the upper layer of oceans. The present review critically assesses the basic knowledge acquired about Prochlorococcus both in the ocean and in the laboratory.     

A likely role for anoxygenic photosynthetic microbes in the formation of ancient stromatolites

Although cyanobacteria are the dominant primary producers in modern stromatolites and other microbialites, the oldest stromatolites pre-date geochemical evidence for oxygenic photosynthesis and cyanobacteria in the rock record. As a step towards the development of laboratory models of stromatolite growth, we tested the potential of a metabolically ancient anoxygenic photosynthetic bacterium to build stromatolites. This organism, Rhodopseudomonas palustris, stimulates the precipitation of calcite in solutions already highly saturated with respect to calcium carbonate, and greatly facilitates the incorporation of carbonate grains into proto-lamina (i.e. crusts). The appreciable stimulation of the growth of proto-lamina by a nonfilamentous anoxygenic microbe suggests that similar microbes may have played a greater role in the formation of Archean stromatolites than previously assumed.     

The role of siderophores in iron acquisition by photosynthetic marine microorganisms

The photosynthetic picocyanobacteria and eukaryotic microorganisms that inhabit the open ocean must be able to supply iron for their photosynthetic and respiratory needs from the subnanomolar concentrations available in seawater. Neither group appears to produce siderophores, although some coastal cyanobacteria do. This is interpreted as an adaptation to the dilute oceanic environment rather than a phylogenetic constraint, since there are cases in which related taxa from different environments have the capacity to produce siderophores. Most photosynthetic marine microorganisms are presumably, however, capable of accessing iron from strong chelates since the majority of dissolved iron in seawater is complexed by organic ligands, including siderophores. Rather than direct internalization of siderophores and other iron chelates, marine organisms primarily appear to use uptake pathways that involve a reduction step to free bound iron, closely coupled with transport into the cell.     

Flow cytometric characterization of marine microbes

The analysis of marine phytoplankton using flow cytometry has enabled the discovery of new taxa and has contributed new understanding to the dynamics and ecological contributions of phytoplankton to the global carbon cycle. Marine phytoplankton are uniquely suited to analysis by flow cytometry because of their size, pigment content, and ability to remain in suspension. Cytometric analysis of marine populations is not without challenges. Phytoplankton communities span a broad range of sizes. The smallest microbes are a few tenths of a micron, while the largest are a few tenths of a millimeter. The improvement of cytometric measurements of scattered laser light allows one to investigate marine microbes whose sizes span several orders of magnitude. To effectively leverage the advantages that marine microbes possess, cytometers have to be carefully engineered for marine use.     

Genome sequence completed of Alcanivorax borkumensis, a hydrocarbon-degrading bacterium that plays a global role in oil removal from marine systems

In this paper, we provide background to the genome sequencing project of Alcanivorax borkumensis, which is a marine bacterium that uses exclusively petroleum oil hydrocarbons as sources of carbon and energy (therefore designated "hydrocarbonoclastic"). It is found in low numbers in all oceans of the world and in high numbers in oil-contaminated waters. Its ubiquity and unusual physiology suggest it is globally important in the removal of hydrocarbons from polluted marine systems. A functional genomics analysis of Alcanivorax borkumensis strain SK2 was recently initiated, and its genome sequence has just been completed. Annotation of the genome, metabolome modelling, and functional genomics, will soon reveal important insights into the genomic basis of the properties and physiology of this fascinating and globally important bacterium.     

Evolution of acidocalcisomes and their role in polyphosphate storage and osmoregulation in eukaryotic microbes

Acidocalcisomes are acidic electron-dense organelles, rich in polyphosphate (poly P) complexed with calcium and other cations. While its matrix contains enzymes related to poly P metabolism, the membrane of the acidocalcisomes has a number of pumps (Ca²⁺-ATPase, V-H⁺-ATPase, H⁺-PPase), exchangers (Na⁺/H⁺, Ca²⁺/H⁺), and at least one channel (aquaporin). Acidocalcisomes are present in both prokaryotes and eukaryotes and are an important storage of cations and phosphorus. They also play an important role in osmoregulation and interact with the contractile vacuole complex in a number of eukaryotic microbes. Acidocalcisomes resemble lysosome-related organelles (LRO) from mammalian cells in many of their properties. They share similar morphological characteristics, acidic properties, phosphorus contents and a system for targeting of their membrane proteins through adaptor complex-3 (AP-3). Storage of phosphate and cations may represent the ancestral physiological function of acidocalcisomes, with cation and pH homeostasis and osmoregulatory functions derived following the divergence of prokaryotes and eukaryotes.     

木质纤维素酶高产菌株的筛选及其对玉米秸秆降解效果的影响

为了提高玉米秸秆中木质素的降解率,从腐烂的树枝和土壤中筛选木质纤维素酶高产菌株,以秸秆为唯一C源富集培养后,采用PDA-愈创木酚法进行初筛,筛选出产木质素酶真菌5株,然后以玉米秸秆为主要C源进行固态发酵和复筛。结果表明:第5号菌株在发酵玉米秸秆5 d后,使木质素的降解率达到最高(34.95%),粗纤维的降解率达到20.00%,显著高于其他4种菌株(P<0.05),其羧甲基纤维素酶比酶活达到116.35 U/g;10 d后,其木质素酶比酶活达到最高(45.64 U/g)。     

动物及其肠道菌群的协同进化研究

动物自身合成一些关键营养物质的能力缺失,转而依赖体内的共生物来完成相应功能,如动物体内共生细菌能帮助宿主从食物中提取营养物质,并能合成一些关键代谢反应的化合物。结合国内外在动物及其肠道菌群的协同进化的研究进展,从三个方面进行了归纳:(1)动物及其肠道微生物组成与功能的协同进化研究;(2)动物行为与肠道微生物的关系;(3)共生肠道微生物在人类或动物自身消化食物、营养获取、健康和疾病方面发挥的重要作用。     

Patterns and mechanisms of genetic and phenotypic differentiation in marine microbes

Microbes in the ocean dominate biogeochemical processes and are far more diverse than anticipated. Thus, in order to understand the ocean system, we need to delineate microbial populations with predictable ecological functions. Recent observations suggest that ocean communities comprise diverse groups of bacteria organized into genotypic (and phenotypic) clusters of closely related organisms. Although such patterns are similar to metazoan communities, the underlying mechanisms for microbial communities may differ substantially. Indeed, the potential among ocean microbes for vast population sizes, extensive migration and both homologous and illegitimate genetic recombinations, which are uncoupled from reproduction, challenges classical population models primarily developed for sexually reproducing animals. We examine possible mechanisms leading to the formation of genotypic clusters and consider alternative population genetic models for differentiation at individual loci as well as gene content at the level of whole genomes. We further suggest that ocean bacteria follow at least two different adaptive strategies, which constrain rates and bounds of evolutionary processes: the 'opportunitroph', exploiting spatially and temporally variable resources; and the passive oligotroph, efficiently using low nutrient concentrations. These ecological lifestyle differences may represent a fundamental divide with major consequences for growth and predation rates, genome evolution and population diversity, as emergent properties driving the division of labour within microbial communities.     

The phylogeny of endolithic microbes associated with marine basalts

We examined the phylogenetic diversity of microbial communities associated with marine basalts, using over 300 publicly available 16S rDNA sequences and new sequence data from basalt enrichment cultures. Phylogenetic analysis provided support for 11 monophyletic clades originating from ocean crust (sediment, basalt and gabbro). Seven of the ocean crust clades (OCC) are bacterial, while the remaining four OCC are in the Marine Group I (MGI) Crenarchaeota. Most of the OCC were found at diverse geographic sites, suggesting that these microorganisms have cosmopolitan distributions. One OCC in the Crenarchaeota consisted of sequences derived entirely from basalts. The remaining OCC were found in both basalts and sediments. The MGI Crenarchaeota were observed in all studies where archaeal diversity was evaluated. These results demonstrate that basalts are occupied by cosmopolitan clades of microorganisms that are also found in marine sediments but are distinct from microorganisms found in other marine habitats, and that one OCC in the ubiquitous MGI Crenarchaeota clade may be an ecotype specifically adapted to basalt.     

8株光合细菌的鉴定及其系统进化关系分析

目的为8株光合细菌(photosynthetic bacteria,PSB)作为益生菌株提供系统资料。方法用常规方法对8株PSB菌株的形态、培养特性及生理生化特征进行鉴定,同时定性分析菌株产生的类胡萝卜素和CoQ,测定菌株16S DNA序列并分析其系统进化关系,在GenBank中获取了8个16S DNA序列号。结果菌株鉴定结果表明:菌株2C、2c和13ing为沼泽红假单胞菌,Ga、Il106、WS8N为类球红细菌,MT1131为荚膜红细菌,rub为深红红螺菌。基于菌株16S DNA序列的系统进化树显示,同一种菌并不总是聚为一簇,但相隔较近;种属完全不同的菌株,尽管序列相似性高达97%以上,在系统进化树上相隔较远。结论8株PSB菌株的鉴定和系统进化关系分析结果为后续研究提供了背景资料,同时菌株在GenBank中获得的16S DNA序列号为菌株作上了生物标记,也为菌株的产权保护提供了依据。     

The dual role of microbes in corrosion

Corrosion is the result of a series of chemical, physical and (micro) biological processes leading to the deterioration of materials such as steel and stone. It is a world-wide problem with great societal and economic consequences. Current corrosion control strategies based on chemically produced products are under increasing pressure of stringent environmental regulations. Furthermore, they are rather inefficient. Therefore, there is an urgent need for environmentally friendly and sustainable corrosion control strategies. The mechanisms of microbially influenced corrosion and microbially influenced corrosion inhibition are not completely understood, because they cannot be linked to a single biochemical reaction or specific microbial species or groups. Corrosion is influenced by the complex processes of different microorganisms performing different electrochemical reactions and secreting proteins and metabolites that can have secondary effects. Information on the identity and role of microbial communities that are related to corrosion and corrosion inhibition in different materials and in different environments is scarce. As some microorganisms are able to both cause and inhibit corrosion, we pay particular interest to their potential role as corrosion-controlling agents. We show interesting interfaces in which scientists from different disciplines such as microbiology, engineering and art conservation can collaborate to find solutions to the problems caused by corrosion.     

Hopanoids in marine cyanobacteria: probing their phylogenetic distribution and biological role

Cyanobacteria are key players in the global carbon and nitrogen cycles and are thought to have been responsible for the initial rise of atmospheric oxygen during the Neoarchean. There is evidence that a class of membrane lipids known as hopanoids serve as biomarkers for bacteria, including many cyanobacteria, in the environment and in the geologic record. However, the taxonomic distributions and physiological roles of hopanoids in marine cyanobacteria remain unclear. We examined the distribution of bacteriohopanepolyols (BHPs) in a collection of marine cyanobacterial enrichment and pure cultures and investigated the relationship between the cellular abundance of BHPs and nitrogen limitation in Crocosphaera watsonii, a globally significant nitrogen‐fixing cyanobacterium. In pure culture, BHPs were only detected in species capable of nitrogen fixation, implicating hopanoids as potential markers for diazotrophy in the oceans. The enrichment cultures we examined exhibited a higher degree of BHP diversity, demonstrating that there are presently unaccounted for marine bacteria, possibly cyanobacteria, associated with the production of a range of BHP structures. Crocosphaera watsonii exhibited high membrane hopanoid content consistent with the idea that hopanoids have an important effect on the bulk physical properties of the membrane. However, the abundance of BHPs in C. watsonii did not vary considerably when grown under nitrogen‐limiting and nitrogen‐replete conditions, suggesting that the role of hopanoids in this organism is not directly related to the physiology of nitrogen fixation. Alternatively, we propose that high hopanoid content in C. watsonii may serve to reduce membrane permeability to antimicrobial toxins in the environment.     

Vegetation-atmosphere interactions and their role in global warming during the latest Cretaceous

Forest vegetation has the ability to warm Recent climate by its effects on albedo and atmospheric water vapour, but the role of vegetation in warming climates of the geologic past is poorly understood. This study evaluates the role of forest vegetation in maintaining warm climates of the Late Cretaceous by (1) reconstructing global palaeovegetation for the latest Cretaceous (Maastrichtian); (2) modelling latest Cretaceous climate under unvegetated conditions and different distributions of palaeovegetation; and (3) comparing model output with a global database of palaeoclimatic indicators. Simulation of Maastrichtian climate with the land surface coded as bare soil produces high-latitude temperatures that are too cold to explain the documented palaeogeographic distribution of forest and woodland vegetation. In contrast, simulations that include forest vegetation at high latitudes show significantly warmer temperatures that are sufficient to explain the widespread geographic distribution of high-latitude deciduous forests. These warmer temperatures result from decreased albedo and feedbacks between the land surface and adjacent oceans. Prescribing a realistic distribution of palaeovegetation in model simulations produces the best agreement between simulated climate and the geologic record of palaeoclimatic indicators. Positive feedbacks between high-latitude forests, the atmosphere, and ocean contributed significantly to high-latitude warming during the latest Cretaceous, and imply that high-latitude forest vegetation was an important source of polar warmth during other warm periods of geologic history.