Ocean and coastal acidification off New England and Nova Scotia

Author Posting. © The Oceanography Society, 2015. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 28, no. 2 (2015): 182-197, doi:10.5670/oceanog.2015.41.New England coastal and adjacent Nova Scotia shelf waters have a reduced buffering capacity because of significant freshwater input, making the region’s waters potentially more vulnerable to coastal acidification. Nutrient loading and heavy precipitation events further acidify the region’s poorly buffered coastal waters. Despite the apparent vulnerability of these waters, and fisheries’ and mariculture’s significant dependence on calcifying species, the community lacks the ability to confidently predict how the region’s ecosystems will respond to continued ocean and coastal acidification. Here, we discuss ocean and coastal acidification processes specific to New England coastal and Nova Scotia shelf waters and review current understanding of the biological consequences most relevant to the region. We also identify key research and monitoring needs to be addressed and highlight existing capacities that should be leveraged to advance a regional understanding of ocean and coastal acidification.This project was supported in part by an appointment to the Internship/Research Participation Program at the Office of Water, US Environmental Protection Agency (EPA), administered by the Oak Ridge Institute for Science and Education through an interagency agreement between the US Department of Energy and the EPA. JS acknowledges support from NASA grant from NNX14AL84G NASA-CCS

Epistatic Roles for Pseudomonas aeruginosa MutS and DinB (DNA Pol IV) in Coping with Reactive Oxygen Species-Induced DNA Damage

Pseudomonas aeruginosa is especially adept at colonizing the airways of individuals afflicted with the autosomal recessive disease cystic fibrosis (CF). CF patients suffer from chronic airway inflammation, which contributes to lung deterioration. Once established in the airways, P. aeruginosa continuously adapts to the changing environment, in part through acquisition of beneficial mutations via a process termed pathoadaptation. MutS and DinB are proposed to play opposing roles in P. aeruginosa pathoadaptation: MutS acts in replication-coupled mismatch repair, which acts to limit spontaneous mutations; in contrast, DinB (DNA polymerase IV) catalyzes error-prone bypass of DNA lesions, contributing to mutations. As part of an ongoing effort to understand mechanisms underlying P. aeruginosa pathoadaptation, we characterized hydrogen peroxide (H2O2)-induced phenotypes of isogenic P. aeruginosa strains bearing different combinations of mutS and dinB alleles. Our results demonstrate an unexpected epistatic relationship between mutS and dinB with respect to H2O2-induced cell killing involving error-prone repair and/or tolerance of oxidized DNA lesions. In striking contrast to these error-prone roles, both MutS and DinB played largely accurate roles in coping with DNA lesions induced by ultraviolet light, mitomycin C, or 4-nitroquinilone 1-oxide. Models discussing roles for MutS and DinB functionality in DNA damage-induced mutagenesis, particularly during CF airway colonization and subsequent P. aeruginosa pathoadaptation are discussed

Role of Adenosine 5‘-Triphosphate Hydrolysis in The Assembly of The Bacteriophage T4 DNA Replication Holoenzyme Complex

Steady-state and pre-steady-state rates of ATP hydrolysis by the 44/62 accessory protein were determined to elucidate the role of ATP hydrolysis in bacteriophage T4 holoenzyme complex formation. Steady-state ATPase measurements of the 44/62 protein under various combinations of 45 protein, DNA substrate, and T4 exo- polymerase indicate that although the 44/62 protein synergistically hydrolyzes ATP in the presence of 45 protein and DNA substrate, the ATPase activity of 44/62 is diminished substantially upon the formation of the holoenzyme complex. The decrease in activity is primarily in kcat while the Km for ATP is changed unsubstantially by the various combinations. Data suggest that the decrease in the rate of ATP hydrolysis upon the addition of T4 exo- polymerase in the presence of 45 protein and DNA substrate is due to formation of a stable holoenzyme complex consisting of only the 45 protein and T4 exo- polymerase in a 1:1 ratio. The 44/62 protein acts catalytically to load 45 protein onto the DNA substrate and does not remain a component of the holoenzyme complex. Pre-steady-state kinetic analysis of the ATP hydrolysis reaction catalyzed by the 44/62 protein loading the 45 protein onto the DNA substrate in the absence or presence of polymerase is biphasic, in which a burst in ATP hydrolysis precedes the steady-state rate of ATP hydrolysis. An identical burst in ATP consumption is obtained under either condition, indicating that ATP hydrolysis is not required to load polymerase into the holoenzyme complex. The data suggest one turnover of ATP at each of the four ATPase active sites of the 44/62 protein per 45 protein loaded. ATP hydrolysis by the 44/62 protein under conditions of holoenzyme complex formation is the rate-limiting step in holoenzyme complex formation. The process of holoenzyme formation appears to be identical for leading and lagging strand synthesis