Spatio-Temporal Characterization of Pinniped Strandings and Human Interaction Cases in the Pacific Northwest, 1991-2016

2018 ◽  
Vol 44 (3) ◽  
pp. 299-318 ◽  
Author(s):  
Amanda J. Warlick ◽  
Deborah A. Duffield ◽  
Dyanna M. Lambourn ◽  
Steven J. Jeffries ◽  
James M. Rice ◽  
...  
2002 ◽  
Vol 58 (3) ◽  
pp. 226-233 ◽  
Author(s):  
Paul A. Knapp ◽  
Henri D. Grissino-Mayer ◽  
Peter T. Soulé

AbstractTree-ring records from western juniper (Juniperus occidentalis var. occidentalis Hook.) growing throughout the interior Pacific Northwest identify extreme climatic pointer years (CPYs) (i.e., severe single-year droughts) from 1500–1998. Widespread and extreme CPYs were concentrated in the 16th and early part of the 17th centuries and did not occur again until the early 20th century. The 217-yr absence of extreme CPYs may have occurred during an extended period of low variance in the Pacific Decadal Oscillation. We mapped climatic boundaries for the interior Pacific Northwest based on the location of sites with similar precipitation variability indices. Three regions, the Northwest (based on chronologies from nine sites), the Southwest (four sites), and the East (five sites) were identified. Our results suggest that western juniper radial growth indices have substantial interannual variability within the northwestern range of the species (central Oregon), particularly when compared with western juniper growing in its eastern range (eastern Oregon, southeastern Idaho, and northern Nevada) and southwestern range (southern Oregon and northeast California). We suspect that the substantial differences in the variability of western juniper radial growth indices are linked to the influence of ENSO events on winter/spring precipitation amounts.


1971 ◽  
Vol 1 (2) ◽  
pp. 261-282 ◽  
Author(s):  
Keith Randle ◽  
Gordon G. Goles ◽  
Laurence R. Kittleman

Twenty-nine samples of volcanic ash from the Pacific Northwest were analyzed by instrumental neutron activation techniques, with the aim of distinguishing among ashes from different sources. Preliminary results of petrographic studies of 42 ash or pumice samples are also reported. Geochemical characteristics of Mazama ash are defined, and problems induced by winnowing of crystalline material during transport and by weathering are discussed. Contents of La, Th, and Co, and La/Yb ratios are shown to be good discriminants. Data on refractive indices and on proportions of crystalline materials also aid in distinguishing among the various volcanic ashes studied. Ash and pumice found in archaeological contexts at Fort Rock Cave, Paisley Cave, Wildcat Canyon, and Hobo Cave are all from Mount Mazama, presumably from the culminating cruption of 7000 years ago.


Author(s):  
Fd Alexandre Sebastião ◽  
K Shahin ◽  
BR LaFrentz ◽  
MJ Griffin ◽  
TP Loch ◽  
...  

2020 ◽  
Vol 112 (1) ◽  
pp. 228-240 ◽  
Author(s):  
Bikash Ghimire ◽  
Scot H. Hulbert ◽  
Camille M. Steber ◽  
Kim Garland‐Campbell ◽  
Karen A. Sanguinet

2006 ◽  
Vol 73 (5) ◽  
pp. 1433-1443 ◽  
Author(s):  
Sarah E. Kidd ◽  
Yat Chow ◽  
Sunny Mak ◽  
Paxton J. Bach ◽  
Huiming Chen ◽  
...  

ABSTRACT Cryptococcus gattii has recently emerged as a primary pathogen of humans and wild and domesticated animals in British Columbia, particularly on Vancouver Island. C. gattii infections are typically infections of the pulmonary and/or the central nervous system, and the incidence of infection in British Columbia is currently the highest reported globally. Prior to this emergence, the environmental distribution of and the extent of colonization by C. gattii in British Columbia were unknown. We characterized the environmental sources and potential determinants of colonization in British Columbia. C. gattii was isolated from tree surfaces, soil, air, freshwater, and seawater, and no seasonal prevalence was observed. The C. gattii concentrations in air samples were significantly higher during the warm, dry summer months, although potentially infectious propagules (<3.3 μm in diameter) were present throughout the year. Positive samples were obtained from many different areas of British Columbia, and some locations were colonization “hot spots.” C. gattii was generally isolated from acidic soil, and geographic differences in soil pH may influence the extent of colonization. C. gattii soil colonization also was associated with low moisture and low organic carbon contents. Most of the C. gattii isolates recovered belonged to the VGIIa genetic subtype; however, sympatric colonization by the VGIIb strain was observed at most locations. At one sampling site, VGIIa, VGIIb, VGI, and the Cryptococcus neoformans serotype AD hybrid all were coisolated. Our findings indicate extensive colonization by C. gattii within British Columbia and highlight an expansion of the ecological niche of this pathogen.


1985 ◽  
Author(s):  
K.B. Olsen ◽  
J.C. Evans ◽  
D.S. Sklarew ◽  
D.C. Girvin ◽  
C.L. Nelson ◽  
...  

2014 ◽  
Vol 15 (2) ◽  
pp. 55-56 ◽  
Author(s):  
Sierra N. Wolfenbarger ◽  
Emily B. Eck ◽  
David H. Gent

Hop powdery mildew, caused by Podosphaera macularis, is an important disease in the Pacific Northwest. Resistant cultivars of hop have been developed and have provided field immunity to the disease until virulent strains of P. macularis emerged. Due to the increase of powdery mildew on formerly resistant cultivars, studies were conducted to characterize potential sources of host resistance. Accepted for publication 5 February 2014. Published 27 March 2014.


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