Polar Microalgae: New Approaches towards Understanding Adaptations to an Extreme and Changing Environment

Polar Regions are unique and highly prolific ecosystems characterized by extreme environmental gradients. Photosynthetic autotrophs, the base of the food web, have had to adapt physiological mechanisms to maintain growth, reproduction and metabolic activity despite environmental conditions that would shut-down cellular processes in most organisms. High latitudes are characterized by temperatures below the freezing point, complete darkness in winter and continuous light and high UV in the summer. Additionally, sea-ice, an ecological niche exploited by microbes during the long winter seasons when the ocean and land freezes over, is characterized by large salinity fluctuations, limited gas exchange, and highly oxic conditions. The last decade has been an exciting period of insights into the molecular mechanisms behind adaptation of microalgae to the cryosphere facilitated by the advancement of new scientific tools, particularly “omics” techniques. We review recent insights derived from genomics, transcriptomics, and proteomics studies. Genes, proteins and pathways identified from these highly adaptable polar microbes have far-reaching biotechnological applications. Furthermore, they may provide insights into life outside this planet, as well as glimpses into the past. High latitude regions also have disproportionately large inputs into global biogeochemical cycles and are the region most sensitive to climate change

Adelina DiTullio\u27s Portfolio

My name is Adelina DiTullio, a student at Duquesne University studying Early Childhood Education. I am an incoming senior and expected to graduate in the Spring of 2021. My portfolio is a collection of work I have produced throughout my academic career in the School of Education at Duquesne University. This portfolio is an assembly of my experiences in the field and training in the classrooms, ranging from kindergarten to fifth grade in all subjects. Included in this portfolio are the modes and assignments that have guided and shaped me into the learning theorist I am today. Through lesson plans, personal teaching statements, and a variety of teaching resources I have created, my portfolio encompasses the type of teacher I hope to become, as well as, the reasons and rationales pushing me toward the field of education. Additionally, included in this portfolio are assignment pieces, infographics, and a variety of lesson plans, all in which I have created to better understand the pedagogy of Early Childhood Education. Personal touches, such as an introductory letter and video and teaching statements were also included to further brand this portfolio, showcasing my individualized path toward becoming an educator and the educator I aspire to become. The creation of my portfolio was intended to be built and improved upon as my studies continue, adding more content and resources as I learn. Through this portfolio, I hope it becomes apparent the depth of the education program at Duquesne University, particularly the complexity of learning that is required. I have been truly blessed with opportunities and experiences from my studies at Duquesne and will continue to learn and grow as an educator while finishing my degree and furthering my education career.https://dsc.duq.edu/portfolios/1015/thumbnail.jp

TREX1 DNA exonuclease deficiency, accumulation of single stranded DNA and complex human genetic disorders

Aicardi-Goutieres syndrome (AGS) is an unusual condition that clinically mimics a congenital viral infection. Several genes have recently been implicated in the aetiology of this disorder. One of these genes encodes the DNA exonuclease TREX1. Recent work from Yang, Lindahl and Barnes has provided insight into the cellular consequence of TREX1-deficiency. They found that TREX1-deficiency resulted in the intracellular accumulation of single stranded DNA resulting in chronic activation of the DNA damage response network, even in cells from Trex1-mutated AGS patients. Here, I summarise their findings and discuss them in context with the other AGS causative genes which encode subunits of the RNase H2 complex. I describe mechanisms by which the inappropriate intracellular accumulation of nucleic acid species might deleteriously impact upon normal cell cycle progression. Finally, using the example of Systemic Lupus Erythematosus (SLE), I also summarise the evidence suggesting that the failure to process intermediates of nucleic acid metabolism can result in the activation of uncontrolled autoimmunity

An Examination of Planning and Implementing Brain-Based Strategies in the Elementary Classroom

Brain-based learning can positively impact student motivation, attitudes and academic achievement. Much of the research is situated in a quantitative paradigm designed to measure motivation, attitudes toward learning, and academic achievement. The purpose of the study was to investigate the extent to which teachers are aware of brain-based learning theory and applying the concepts of the theory to their teaching. The qualitative study utilized brain-based learning theory as a research framework. The study employed a semi-structured, face-to-face interview method to gain a better understanding of what information teachers currently know about brain-based learning and what they need in order to create classrooms that implement curriculum using brain-based learning theory. The study also explored the extent to which teachers learned about brain-based learning theory in their teacher preparation programs. The study has implications for pedagogy as well as curriculum choices in school districts and teacher preparation programs. Findings include evidence that teachers had little knowledge of brain-based learning theory unless they had engaged in professional development specific to brain-based learning. However, teachers often unknowingly implemented brain-based learning strategies. Findings also include evidence that teachers did not recall learning about brain-based learning theory in their teacher preparation programs. The study includes recommendations for general education teachers, higher education faculty and future research

Colony formation in Phaeocystis antarctica : connecting molecular mechanisms with iron biogeochemistry

© The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Biogeosciences 15 (2018): 4923-4942, doi:10.5194/bg-15-4923-2018.Phaeocystis antarctica is an important phytoplankter of the Ross Sea where it dominates the early season bloom after sea ice retreat and is a major contributor to carbon export. The factors that influence Phaeocystis colony formation and the resultant Ross Sea bloom initiation have been of great scientific interest, yet there is little known about the underlying mechanisms responsible for these phenomena. Here, we present laboratory and field studies on Phaeocystis antarctica grown under multiple iron conditions using a coupled proteomic and transcriptomic approach. P. antarctica had a lower iron limitation threshold than a Ross Sea diatom Chaetoceros sp., and at increased iron nutrition (>120pM Fe') a shift from flagellate cells to a majority of colonial cells in P. antarctica was observed, implying a role for iron as a trigger for colony formation. Proteome analysis revealed an extensive and coordinated shift in proteome structure linked to iron availability and life cycle transitions with 327 and 436 proteins measured as significantly different between low and high iron in strains 1871 and 1374, respectively. The enzymes flavodoxin and plastocyanin that can functionally replace iron metalloenzymes were observed at low iron treatments consistent with cellular iron-sparing strategies, with plastocyanin having a larger dynamic range. The numerous isoforms of the putative iron-starvation-induced protein (ISIP) group (ISIP2A and ISIP3) had abundance patterns coinciding with that of either low or high iron (and coincident flagellate or the colonial cell types in strain 1871), implying that there may be specific iron acquisition systems for each life cycle type. The proteome analysis also revealed numerous structural proteins associated with each cell type: within flagellate cells actin and tubulin from flagella and haptonema structures as well as a suite of calcium-binding proteins with EF domains were observed. In the colony-dominated samples a variety of structural proteins were observed that are also often found in multicellular organisms including spondins, lectins, fibrillins, and glycoproteins with von Willebrand domains. A large number of proteins of unknown function were identified that became abundant at either high or low iron availability. These results were compared to the first metaproteomic analysis of a Ross Sea Phaeocystis bloom to connect the mechanistic information to the in situ ecology and biogeochemistry. Proteins associated with both flagellate and colonial cells were observed in the bloom sample consistent with the need for both cell types within a growing bloom. Bacterial iron storage and B12 biosynthesis proteins were also observed consistent with chemical synergies within the colony microbiome to cope with the biogeochemical conditions. Together these responses reveal a complex, highly coordinated effort by P. antarctica to regulate its phenotype at the molecular level in response to iron and provide a window into the biology, ecology, and biogeochemistry of this group.Support for this study was provided by an Investigator grant to Mak A. Saito from the Gordon and Betty Moore Foundation (GBMF3782), National Science Foundation grants NSF-PLR 0732665, OCE-1435056, OCE-1220484, and ANT-1643684, the WHOI Coastal Ocean Institute, and a CINAR Postdoctoral Scholar Fellowship provided to Sara J. Bender through the Woods Hole Oceanographic Institution. Support was provided to Andrew E. Allen through NSF awards ANT-0732822, ANT-1043671, and OCE-1136477 and Gordon and Betty Moore Foundation grant GBMF3828. Additional support was provided to GRD through NSF award OPP-0338097

The multiple fates of sinking particles in the North Atlantic Ocean

Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 29 (2015): 1471–1494, doi:10.1002/2014GB005037.The direct respiration of sinking organic matter by attached bacteria is often invoked as the dominant sink for settling particles in the mesopelagic ocean. However, other processes, such as enzymatic solubilization and mechanical disaggregation, also contribute to particle flux attenuation by transferring organic matter to the water column. Here we use observations from the North Atlantic Ocean, coupled to sensitivity analyses of a simple model, to assess the relative importance of particle-attached microbial respiration compared to the other processes that can degrade sinking particles. The observed carbon fluxes, bacterial production rates, and respiration by water column and particle-attached microbial communities each spanned more than an order of magnitude. Rates of substrate-specific respiration on sinking particle material ranged from 0.007 ± 0.003 to 0.173 ± 0.105 day−1. A comparison of these substrate-specific respiration rates with model results suggested sinking particle material was transferred to the water column by various biological and mechanical processes nearly 3.5 times as fast as it was directly respired. This finding, coupled with strong metabolic demand imposed by measurements of water column respiration (729.3 ± 266.0 mg C m−2 d−1, on average, over the 50 to 150 m depth interval), suggested a large fraction of the organic matter evolved from sinking particles ultimately met its fate through subsequent remineralization in the water column. At three sites, we also measured very low bacterial growth efficiencies and large discrepancies between depth-integrated mesopelagic respiration and carbon inputs.U.S. Environmental Protection Agency (EPA) STAR Grant Number: FP-91744301-0; National Science Foundation Grant Numbers OCE-1061883, EF-0424599, OCE-1155438, OCE-1059884, OCE-1031143; Gordon and Betty Moore Foundation Grant Numbers: 3301, 3789; Gordon and Betty Moore Foundation; Woods Hole Oceanographic Institution2016-03-2

Iron limitation of a springtime bacterial and phytoplankton community in the Ross Sea : implications for vitamin B12 nutrition

© The Author(s), 2011. This is an open-access article subject to a non-exclusive license between the authors and Frontiers Media SA, which permits use, distribution and reproduction in other forums. The definitive version was published in Frontiers in Microbiology 2 (2011): 160, doi:10.3389/fmicb.2011.00160.The Ross Sea is home to some of the largest phytoplankton blooms in the Southern Ocean. Primary production in this system has previously been shown to be iron limited in the summer and periodically iron and vitamin B12 colimited. In this study, we examined trace metal limitation of biological activity in the Ross Sea in the austral spring and considered possible implications for vitamin B12 nutrition. Bottle incubation experiments demonstrated that iron limited phytoplankton growth in the austral spring while B12, cobalt, and zinc did not. This is the first demonstration of iron limitation in a Phaeocystis antarctica-dominated, early season Ross Sea phytoplankton community. The lack of B12 limitation in this location is consistent with previous Ross Sea studies in the austral summer, wherein vitamin additions did not stimulate P. antarctica growth and B12 was limiting only when bacterial abundance was low. Bottle incubation experiments and a bacterial regrowth experiment also revealed that iron addition directly enhanced bacterial growth. B12 uptake measurements in natural water samples and in an iron fertilized bottle incubation demonstrated that bacteria serve not only as a source for vitamin B12, but also as a significant sink, and that iron additions enhanced B12 uptake rates in phytoplankton but not bacteria. Additionally, vitamin uptake rates did not become saturated upon the addition of up to 95 pM B12. A rapid B12 uptake rate was observed after 13 min, which then decreased to a slower constant uptake rate over the next 52 h. Results from this study highlight the importance of iron availability in limiting early season Ross Sea phytoplankton growth and suggest that rates of vitamin B12 production and consumption may be impacted by iron availability.This research was supported by NSF grants OCE-0752291, OPP-0440840, OPP-0338097, OPP-0338164, ANT-0732665, OCE-0452883, and OCE-1031271, the Center for Microbial Oceanography Research and Education (CMORE) and a National Science Foundation (NSF) Graduate Research Fellowship (2007037200) and an Environmental Protection Agency STAR Fellowship to EMB (F6E20324)

Temperature-induced viral resistance in Emiliania huxleyi (Prymnesiophyceae)

© The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in PLoS One 9 (2014): e112134, doi:10.1371/journal.pone.0112134.Annual Emiliania huxleyi blooms (along with other coccolithophorid species) play important roles in the global carbon and sulfur cycles. E. huxleyi blooms are routinely terminated by large, host-specific dsDNA viruses, (Emiliania huxleyi Viruses; EhVs), making these host-virus interactions a driving force behind their potential impact on global biogeochemical cycles. Given projected increases in sea surface temperature due to climate change, it is imperative to understand the effects of temperature on E. huxleyi’s susceptibility to viral infection and its production of climatically active dimethylated sulfur species (DSS). Here we demonstrate that a 3°C increase in temperature induces EhV-resistant phenotypes in three E. huxleyi strains and that successful virus infection impacts DSS pool sizes. We also examined cellular polar lipids, given their documented roles in regulating host-virus interactions in this system, and propose that alterations to membrane-bound surface receptors are responsible for the observed temperature-induced resistance. Our findings have potential implications for global biogeochemical cycles in a warming climate and for deciphering the particular mechanism(s) by which some E. huxleyi strains exhibit viral resistance.This study was supported by funding from the National Science Foundation (OCE-1061883 to KDB, BVM, and OCE-1061876 to GRD) and in part by grants from The Gordon and Betty Moore Foundation (to BVM and KDB)

Thaumarchaeal ecotype distributions across the equatorial Pacific Ocean and their potential roles in nitrification and sinking flux attenuation

© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Limnology and Oceanography 62 (2017): 1984–2003, doi:10.1002/lno.10547.Thaumarchaea are among the most abundant microbial groups in the ocean, but controls on their abundance and the distribution and metabolic potential of different subpopulations are poorly constrained. Here, two ecotypes of ammonia-oxidizing thaumarchaea were quantified using ammonia monooxygenase (amoA) genes across the equatorial Pacific Ocean. The shallow, or water column “A” (WCA), ecotype was the most abundant ecotype at the depths of maximum nitrification rates, and its abundance correlated with other biogeochemical indicators of remineralization such as NO3 : Si and total Hg. Metagenomes contained thaumarchaeal genes encoding for the catalytic subunit of the urease enzyme (ureC) at all depths, suggesting that members of both WCA and the deep, water column “B” (WCB) ecotypes may contain ureC. Coupled urea hydrolysis-ammonia oxidation rates were similar to ammonia oxidation rates alone, suggesting that urea could be an important source of ammonia for mesopelagic ammonia oxidizers. Potential inducement of metal limitation of both ammonia oxidation and urea hydrolysis was demonstrated via additions of a strong metal chelator. The water column inventory of WCA was correlated with the depth-integrated abundance of WCB, with both likely controlled by the flux of sinking particulate organic matter, providing strong evidence of vertical connectivity between the ecotypes. Further, depth-integrated amoA gene abundance and nitrification rates were correlated with particulate organic nitrogen flux measured by contemporaneously deployed sediment traps. Together, the results refine our understanding of the controls on thaumarchaeal distributions in the ocean, and provide new insights on the relationship between material flux and microbial communities in the mesopelagic.United States National Science Foundation (NSF) Grant Numbers: OCE-1260006, OCE-1031271, OCE-1337780, OCE-1259994; University of Maryland Center for Environmental Science (UMCES); JGI Community Sequencing Project 133

Legacy Rule Insights and Challenges

Legacy Rule Insights and Challenges Authors Mrs. Arica DiTullio - United States - GAI Consultants, Inc. Ms. Leigh Rounce - United States - GAI Consultants, Inc. Abstract This presentation will provide a summary of the proposed Legacy Impoundment Rule, which includes regulations for inactive impoundments and inactive landfill at inactive facilities. The discussion will include a review of the timeline for the Coal Combustion Residual (CCR) Rule and prudent definitions of terminology, such as Facility, Inactive Facility, Inactive Impoundment, Legacy Impoundment, Inactive Landfill, CCR Unit and CCR Management Unit. Summary and examples of Legacy CCR Surface Impoundment Applicability Documentation will be provided. Legacy impoundments need to implement most measures outlined in the CCR Rule, including inspections, monitoring of instrumentation, reporting, groundwater monitoring and reporting. CCRMUs facility evaluations must be initiated upon effective date of the Final Rule. Facilities must consult available records, complete a physical inspection, and complete necessary field investigations. The Facility Evaluation Report must be completed within 3 months of the Final Rule effective date and must be certified by a qualified professional engineer. This report must contain the results of the facility evaluation and additional information about the CCRMUs onsite. After identifying CCRMUs, facilities are required to implement some other measures outlined in the CCR Rule. The presentation will conclude with highlighting some of the challenges anticipated and hypothetical case examples