The Deepwater Horizon oil spill in the Gulf of Mexico is the deepest and largest offshore spill in the United State history and its impacts on marine ecosystems are largely unknown. Here, we showed that the microbial community functional composition and structure were dramatically altered in a deep-sea oil plume resulting from the spill. A variety of metabolic genes involved in both aerobic and anaerobic hydrocarbon degradation were highly enriched in the plume compared with outside the plume, indicating a great potential for intrinsic bioremediation or natural attenuation in the deep sea. Various other microbial functional genes that are relevant to carbon, nitrogen, phosphorus, sulfur and iron cycling, metal resistance and bacteriophage replication were also enriched in the plume. Together, these results suggest that the indigenous marine microbial communities could have a significant role in biodegradation of oil spills in deep-sea environments.

Micro-organisms play critical roles in many important biogeochemical processes in the Earth's biosphere. However, understanding and characterizing the functional capacity of microbial communities are still difficult due to the extremely diverse and often uncultivable nature of most micro-organisms. In this study, we developed a new functional gene array, GeoChip 4, for analysing the functional diversity, composition, structure, metabolic potential/activity and dynamics of microbial communities. GeoChip 4 contained approximately 82 000 probes covering 141 995 coding sequences from 410 functional gene families related to microbial carbon (C), nitrogen (N), sulphur (S), and phosphorus (P) cycling, energy metabolism, antibiotic resistance, metal resistance/reduction, organic remediation, stress responses, bacteriophage and virulence. A total of 173 archaeal, 4138 bacterial, 404 eukaryotic and 252 viral strains were targeted, providing the ability to analyse targeted functional gene families of micro-organisms included in all four domains. Experimental assessment using different amounts of DNA suggested that as little as 500 ng environmental DNA was required for good hybridization, and the signal intensities detected were well correlated with the DNA amount used. GeoChip 4 was then applied to study the effect of long-term warming on soil microbial communities at a Central Oklahoma site, with results indicating that microbial communities respond to long-term warming by enriching carbon degradation, nutrient cycling (nitrogen and phosphorous) and stress response gene families. To the best of our knowledge, GeoChip 4 is the most comprehensive functional gene array for microbial community analysis.

Accurate climate projections require an understanding of the effects of warming on ecological communities and the underlying mechanisms that drive them 1-3 . However, little is known about the effects of climate warming on the succession of microbial communities 4,5 . Here we examined the temporal succession of soil microbes in a long-term climate change experiment at a tall-grass prairie ecosystem. Experimental warming was found to significantly alter the community structure of bacteria and fungi. By determining the time-decay relationships and the paired differences of microbial communities under warming and ambient conditions, experimental warming was shown to lead to increasingly divergent succession of the soil microbial communities, with possibly higher impacts on fungi than bacteria. Variation partition-and null model-based analyses indicate that stochastic processes played larger roles than deterministic ones in explaining microbial community taxonomic and phylogenetic compositions. However, in warmed soils, the relative importance of stochastic processes decreased over time, indicating a potential deterministic environmental filtering elicited by warming. Although successional trajectories of microbial communities are difficult to predict under future climate change scenarios, their composition and structure are projected to be less variable due to warming-driven selection.

WRKY transcription factors form a large family that plays a role in plant responses to biotic stress and during senescence. Defining in vivo relevant WRKY/promoter relationships has been hampered by the factors' indiscriminate binding to known W box DNA elements and their possible genetic redundance. Employing chromatin immunoprecipitations (ChIP) of cultured cells, we show that parsley (Petroselinum crispum) WRKY1 protein binds to the W boxes of its native promoter as well as to that of PcWRKY3 and the defense-related PR10-class marker gene Pathogenesis-Related1-1 (PcPR1-1). Although present at low concentrations in resting cells, WRKY1 does not appear to play a role in the immediate early gene response upon elicitation because it does not bind to the promoter at this time. Paradoxically, in vivo binding at the PcWRKY1 promoter correlates more with downregulation of gene expression, whereas previous overexpression studies suggested an activating function of WRKY1 on PcWRKY1 expression. By contrast, PcPR1-1 expression remains strong when its promoter is occupied in vivo by WRKY1. Unexpectedly, ChIP revealed that W boxes at promoter sites are constitutively occupied by other WRKY transcription factors, indicating that site recruitment does not seem to play a major role in their regulation. Rather, WRKY proteins very likely act in a network of mutually competing participants with temporal displacement occurring at defined preoccupied sites by other family members in a stimulus-dependent manner.

SummaryBRI1-like receptor kinase (BRL1) was identified as an extragenic suppressor of a weak bri1 allele, bri1-5, in an activation-tagging genetic screen for novel brassinosteroid (BR) signal transduction regulators. BRL1 encodes a leucine-rich repeat receptor-like protein kinase (LRR-RLK). Sequence alignment revealed that BRL1 is closely related to BRI1, which is involved in BR perception. Overexpression of a BRL1 cDNA, driven by a constitutive CaMV 35S promoter, recapitulates the bri1-5 suppression phenotypes, and partially complements the phenotypes of a null bri1 allele, bri1-4. Analysis of a BR-specific feedback response gene, CPD, indicates that BRL1 functions in BR signaling. BRL1 expression pattern overlaps with, but is distinct from, that of BRI1. In addition, both the expression level and in vitro kinase autophosphorylation activity of BRL1 are significantly lower than those of BRI1. bri1-5 brl1-1 double mutant plants have enhanced developmental defects relative to bri1-5 mutant plants, revealing that BRL1 plays a partially redundant role with BRI1 in controlling Arabidopsis growth and development. These findings enhance our understanding of functional redundancy and add an additional layer of complexity to RLK-mediated BR signaling transduction in Arabidopsis.

| Sulphate-reducing microorganisms (SRMs) are a phylogenetically diverse group of anaerobes encompassing distinct physiologies with a broad ecological distribution. As SRMs have important roles in the biogeochemical cycling of carbon, nitrogen, sulphur and various metals, an understanding of how these organisms respond to environmental stresses is of fundamental and practical importance. In this Review, we highlight recent applications of systems biology tools in studying the stress responses of SRMs, particularly Desulfovibrio spp., at the cell, population, community and ecosystem levels. The syntrophic lifestyle of SRMs is also discussed, with a focus on system-level analyses of adaptive mechanisms. Such information is important for understanding the microbiology of the global sulphur cycle and for developing biotechnological applications of SRMs for environmental remediation, energy production, biocorrosion control, wastewater treatment and mineral recovery.

The Arabidopsis BRS1 gene encodes a serine carboxypeptidase II-like protein. Its biological role in the brassinosteroid signaling pathway was first established by its capability to specifically suppress a weak brassinosteroid insensitive 1 (bri1) allele, bri1-5, when overexpressed. To gain additional insights into the molecular mechanisms of BRS1 function, the subcellular localization and the biochemical characteristics of BRS1 were determined by using transgenic plants harboring a 35S-BRS1-GFP construct and fusion proteins purified from 35S-BRS1-FLAG transgenic plants. The BRS1-GFP protein was mainly secreted and accumulated in the extracellular space. Immunological data suggest that BRS1 is proteolytically processed by an unknown endoproteinase in planta. Affinity-purified BRS1-FLAG from transgenic plants show strong hydrolytic activity with a broad P1 substrate preference including basic and hydrophobic groups on either side of the scissile bond. The hydrolytic activity of BRS1 can be strongly inhibited by a serine protease inhibitor, phenylmethylsulfonyl fluoride. The pH and temperature optima for the hydrolytic activity of BRS1 are pH 5.5 and 50°C, respectively. These data demonstrate that BRS1 is a secreted and active serine carboxypeptidase, consistent with the hypothesis suggested by our previous genetic evidence that BRS1 may process a protein involved in an early event in the BRI1 signaling pathway.Serine carboxypeptidases (Ser-CPs) 2 are widely distributed proteases identified in most higher organisms. The major structural characteristic of these proteins is that they contain a conserved amino acid triad, Ser-His-Asp, catalytically essential for enzyme activity (1). In mammals, Ser-CPs are largely involved in producing active peptide hormones from their inactive precursors. This process usually requires two consecutive steps. First, a larger precursor is cleaved at selective sites by an endopeptidase such as prohormone convertase 1, prohormone convertase 2, or furin. The Ser-CPs are then responsible for trimming off the exposed carboxyl-terminal amino acids and transforming the inactive intermediates into active hormones (2, 3).In plants, extensive studies of Ser-CPs have been mainly focused on their functions in turnover and mobilization of storage proteins using as nitrogen and carbon resources during seed germination and senescence (4). Recent studies suggested that plant Ser-CPs may also be involved in various signaling events important for plant growth and development such as programmed cell death, brassinosteroid (BR) signaling, and seed development (5-7). By using a gain-of-function genetic screen we previously identified a putative Ser-CP gene, BRS1, as a bri1 (brassinosteroid insensitive 1) suppressor. Overexpression of BRS1 can suppress bri1 extracellular domain mutations but fails to suppress a kinase-dead bri1 mutant. These results strongly indicate that the bri1 suppression function of BRS1 is dependent on an at least partially functional BRI1 receptor kinase. Analyses of BRS1 protein str...

Determining the temporal scaling of biodiversity, typically described as species-time relationships (STRs), in the face of global climate change is a central issue in ecology because it is fundamental to biodiversity preservation and ecosystem management. However, whether and how climate change affects microbial STRs remains unclear, mainly due to the scarcity of long-term experimental data. Here, we examine the STRs and phylogenetic-time relationships (PTRs) of soil bacteria and fungi in a longterm multifactorial global change experiment with warming (+3 °C), half precipitation (−50%), double precipitation (+100%) and clipping (annual plant biomass removal). Soil bacteria and fungi all exhibited strong STRs and PTRs across the 12 experimental conditions. Strikingly, warming accelerated the bacterial and fungal STR and PTR exponents (that is, the w values), yielding significantly (P < 0.001) higher temporal scaling rates. While the STRs and PTRs were significantly shifted by altered precipitation, clipping and their combinations, warming played the predominant role. In addition, comparison with the previous literature revealed that soil bacteria and fungi had considerably higher overall temporal scaling rates (w = 0.39-0.64) than those of plants and animals (w = 0.21-0.38). Our results on warmingenhanced temporal scaling of microbial biodiversity suggest that the strategies of soil biodiversity preservation and ecosystem management may need to be adjusted in a warmer world.