Supporting diverse Pacific NW marine data access needs via the NANOOS Visualization system (NVS) and data services

Serving PNW users via the ANANOOS Visualization System: Data integration and management

Variability in water column respiration in Salish Sea waters and implications for coastal and ocean acidification

Water column respiration is a key driver of carbon cycling, ocean acidification, and oxygen dynamics in marine ecosystems. However, empirical estimates of the range and variability of respiration and its relative contribution to ocean acidification are seldom measured. In 2014, we began measuring respiration rates at multiple sites in the central Salish Sea (San Juan Islands, Bellingham Bay) and then initiated routine monitoring of water column respiration at multiple sites in Padilla Bay National Estuarine Research Reserve (NERR). Measurements in Padilla Bay were integrated into the well-established NERR System Wide Monitoring Program (SWMP). Our investigation revealed that 1) rates of respiration vary seasonally and appear to be associated with changes in organic matter supply and, to a lesser extent, temperature, and 2) incoming deeper waters of marine origin are characterized by relatively low rates of respiration (i.e. ~5ugO2/L/h). To further explore underlying mechanisms, we conducted a series of manipulative experiments to investigate the direct effect of increasing ocean temperature and organic matter supply on rates of respiration. These experiments revealed that respiration can more than triple in response to increases in organic carbon supply and that this response may be influenced by seasonal changes in the export of organic matter and detritus from the extensive eelgrass meadows of Padilla Bay. Our field sampling and manipulative experiments have produced empirical estimates of respiration that can be included in models and projections of water quality and ocean acidification for the Puget Sound, and provide insight into the response of inland marine waters of the Pacific Northwest to a warmer, more acidified ocean

A NOS1AP gene variant is associated with a paradoxical increase of the QT-interval shortening effect of digoxin

Digoxin is characterized by a small therapeutic window and a QT-interval shortening effect. Moreover, it has been shown that the genetic variants of the nitric oxide synthase-1 adaptor protein (NOS1AP) gene are associated with QT-interval prolongation. We investigated whether the rs10494366 variant of the NOS1AP gene decreases the QT-interval shortening effect of digoxin in patients using this drug. We included 10,057 individuals from the prospective population-based cohort of the Rotterdam Study during a median of 12.2 (interquartile range (IQR) 6.7-18.1) years of follow-up. At study entry, the mean age was 64 years and almost 59% of participants were women. A total of 23,179 ECGs were longitudinally recorded, of which 334 ECGs were from 249 individuals on digoxin therapy. The linear mixed model analysis was used to estimate the effect of the rs10494366 variant on the association between digoxin use and QT-interval duration, adjusted for age, sex, RR interval, diabetes, heart failure, and history of myocardial infarction. In non-users of digoxin, the GG genotype was associated with a significant 6.5 ms [95% confidence interval (CI) 5.5; 7.5] longer QT-interval duration than the TT variant. In current digoxin users, however, the GG variant was associated with a significantly -23.9 [95%CI -29.5; -18.5] ms shorter mean QT-interval duration than in those with the TT variant with -15.9 [95%CI -18.7; -13.1]. This reduction was strongest in the high digoxin dose category [≥0.250 mg/day] with the GG genotype group, with -40.8 [95%CI -52.5; -29.2] ms changes compared to non-users. Our study suggests that the minor homozygous GG genotype group of the NOS1AP gene rs10494366 variant is associated with a paradoxical increase of the QT-interval shortening effect of digoxin in a population of European ancestry

Does Puget Sound have a long-term memory?

More than a decade of high-resolution, full-water column data collected by profiling UW ORCA/NANOOS moorings in several Puget Sound Basins are used to investigate interannual variability of near-surface and deep water properties. Although there are no significant trends in temperature, salinity, density and dissolved oxygen spanning the last decade, measurements show steady and relatively strong trends in these variables over periods of 3 to 5 years in both South Sound near bottom waters and in south Hood Canal deep water. For example, the annual minimum density in south Hood Canal deep water increased four years in a row from 2006 to 2009, then this trend reversed for three years. In Carr Inlet the annual maximum deep temperature increased five years in a row from 2011 to 2015, with deep salinity following a similar trend. As these trends are significantly longer than expected flushing and residence times (\u3c year), this hints at potential interannual dynamical feedbacks, longer-term system “memory”, and/or similar trends in ocean and atmospheric forcing. Using archived National Data Buoy Center, National Weather Service and UW Atmospheric Sciences data we explore and report on potential factors contributing to these trends

Slavery as a national crime: Defining Britishness in Encounters with the Flying Dutchman

Early British gothic fiction has often been analyzed in terms of the religious, political and cultural oppositions it helps to construct between Britain and the European continent, in particular in Catholic countries like France and Spain. One could argue that the cultural work of Gothic in these cases is to (re)define cultural differences between spaces that are geographically already separate. This division of territorial space is obviously much less clear at sea, and so this raises the question if and how national boundaries and identities are being upheld and transgressed in nautical Gothic. The figure of the Flying Dutchman, the ghostly captain doomed to sail the world seas forever, provides and interesting case study for exploring this issue of constructing such national identities. Nineteenth century British culture demonstrates a persistent preoccupation with the ghostly Dutchman. Numerous adaptations and manifestations of the Dutchman in British poetry, fiction, popular song and drama attest to the often problematic ‘Doppelgänger dilemmas’ (Rubright) the Flying Dutchman presents to a British audience: part of his frightening quality is that he is too close for comfort. In my article I will analyze representations of the Flying Dutchman in two British dramas (Fitzball & Taylor), a novel (Marryat), as well as some British poems and songs (1820-1860) in connection to encounters at sea and in the colonies. I will argue that in British nautical gothic the Flying Dutchman often serves as a projection screen for racist attitudes and pro-slavery opinions, but that British characters in these texts do not always succeed in warding off these attitudes

Regional and temporal variability in Puget Sound zooplankton: bottom-up links to juvenile salmon

We use data from the Puget Sound Zooplankton Monitoring Program to explore patterns of spatial and interannual variability in zooplankton communities in response to environmental change during 2014-2017. This program is a collaborative effort involving 10 tribal, county, state, federal, academic, and nonprofit entities initiated via the Salish Sea Marine Survival Project with the goal of understanding the key role of zooplankton in food webs and ecosystems. Large interannual differences in the environment over this period strong effects on zooplankton community structure and abundance. 2014 began as a fairly normal year in Puget Sound until the Pacific Warm Anomaly event nicknamed “The Blob” began to affect the region during late summer and fall. Unprecedented warm anomalies occurred in summer 2015, persisting through 2016. Off the coast of Washington and Oregon, clear effects on zooplankton community structure were observed, with rare oceanic species occurring in coastal samples concurrent with decreased overall biomass. In sharp contrast, few rare species were collected in Puget Sound, and zooplankton increased in 2015 and 2016 relative to 2014, including increases in nearly all taxa that are important juvenile salmon prey. A few taxa, most notably the dinoflagellate Noctiluca and numerous species of small jellyfish, decreased during the warm years, and shifts in the seasonal phenology of some taxa were observed. These and other findings from the Puget Sound Zooplankton Monitoring Program will be presented in the context of the implications of environmental change for juvenile salmon growth and survival

Patterns and variability in ocean acidification conditions in Puget Sound and the Strait of Juan de Fuca

The Washington Ocean Acidification Center is working with NOAA and other partners to increase understanding of ocean acidification dynamics and spatial variability in the Salish Sea, and how these correlate with planktonic responses. These data are critical for assessing water quality, areas with higher or lower OA stress, and to understand effects on the food web. Two main strategies are employed; seasonal ship cruises provide spatial coverage and the ability to collect plankton, while mooring buoys provide information on mechanisms and the range of variation due to the high-resolution and constant coverage they provide. Results show a strong degree of depth, seasonal, and spatial variation in pH and aragonite saturation state. In general, the lowest pH and aragonite saturation state values are at depth, particularly in stratified areas, though this can shift during seasonal localized upwelling, e.g., Southern Hood Canal, and in mixed water columns, e.g., the Main Basin. Seasonal patterns are spatially diverse, with stratified areas exhibiting strong vertical gradients with depth during summer and more homogenous conditions during winter; well-mixed areas show less variation year-round. This implies that species encounter quite different OA conditions in various parts of the Salish Sea between the seasons. Mooring CO2 data reveal higher variation during late fall through early spring at sites within the Salish Sea, due to winter mixing of stratified waters, yet the reverse pattern off the Washington coast, due to summer upwelling. In both cases, these mechanisms (winter mixing and summer upwelling) operate across a gradient, bringing relatively deeper lower pH / aragonite saturation state waters in contact with surface waters with higher values. Such changes in the spatial and depth distribution of corrosive conditions have broad implications for sensitive marine life

Defects in CD4+ T cell LFA‐1 integrin‐dependent adhesion and proliferation protect Cd47−/− mice from EAE

Peer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/141316/1/jlb0493.pd