1,427 research outputs found
Freshwater Plankton Crustacea of the Colville River Area, Northern Alaska
Reports study of Microcrustacea from 200 water bodies, collected during the summer of 1955. Twenty-two species of Cladocera, 29 Copepoda and six larger forms were identified. Some species characteristic of lakes or pools are separated. Surface temperatures ranged from 0.5 to 20.5 C. Chemical determinations of 48 water bodies include chloride, calcium, bicarbonate and oxygen. Similarities with Siberian and other high latitude forms are noted
Disturbed Sediments in a Small Alpine Lake in Colorado
Palynologists, students of paleolimnology and others interested in former ecological conditions may study cores of sediments deposited in present or now-dry lake basins. Undisturbed sequences are crucial to drawing correct inferences from sedimentary records. Recently Nichols called attention to the disruption of tundra pond sediments by blocks of ice floating from the basin bottom to the water surface. This note records the derangement of sediments in a small alpine lake; while the actual disturbance was not witnessed, this type of event may be of frequent occurrence in remote mountainous areas and go unnoticed. Among the lakes receiving limnological study in Rocky Mountain National Park is a small unnamed tarn at the head of Fern Creek, a tributary of the Big Thompson River ...
First Records of Two Neotropical Species of Mesocyclops (Copepoda) from Yukon Territory: Cases of Passive Dispersal?
Two species of neotropical cyclopoid copepod crustaceans, Mesocyclops longisetus curvatus and Mesocyclops venezolanus, were collected from a pond at Shingle Point, Yukon Territory, Canada, in September 1974. This is the first record of M. longisetus curvatus north of the southern United States and the first record of M. venezolanus north of Honduras. We provide amplified descriptions of both species. Four additional congeners, M. americanus, M. edax, M. reidae, and M. ruttneri, are now known from the continental U.S. and Canada. We provide a key to the identification of the six species. We hypothesize that the specimens of M. longisetus curvatus and M. venezolanus may have been passively transported to Shingle Point by migrant shorebirds.Key words: Copepoda, Cyclopoida, Mesocyclops, new record, Yukon, neotropical, zoogeography, passive dispersal, identification keyEn septembre 1974, on a recueilli deux espèces de copépodes cyclopoïdes néogènes, Mesocyclops longisetus curvatus et Mesocyclops venezolanus, dans un étang situé à Shingle Point, dans le territoire du Yukon au Canada. Cela représente la première occurrence rapportée de M. longisetus curvatus au nord de la partie méridionale des États-Unis, et la première de M. venezolanus au nord du Honduras. On donne une description détaillée des deux espèces. On sait maintenant qu'il existe quatre autres congénères, M. americanus, M. edax, M. reida et M. ruttneri, aux États-Unis américains et au Canada. On fournit un code permettant d'identifier les six espèces. On émet l'hypothèse que les spécimens de M. longisetus curvatus et de M. venezolanus ont pu être transportés de façon passive à Shingle Point par des oiseaux de rivage migrateurs.Mots clés: copépodes, cyclopoïdes, Mesocyclops, nouvelle Occurrence rapportée, Yukon, néogène, zoogéographie, dispersion passive, code d'identificatio
Oregon 2100: projected climatic and ecological changes
Greenhouse climatic warming is underway and exacerbated by human activities. Future outcomes of these processes can be projected using computer models checked against climatic changes during comparable past atmospheric compositions. This study gives concise quantitative predictions for future climate, landscapes, soils, vegetation, and marine and terrestrial animals of Oregon. Fossil fuel burning and other human activities by the year 2100 are projected to yield atmospheric CO2 levels of about 600-850 ppm (SRES A1B and B1), well above current levels of 400 ppm and preindustrial levels of 280 ppm. Such a greenhouse climate was last recorded in Oregon during the middle Miocene, some 16 million years ago. Oregon’s future may be guided by fossil records of the middle Miocene, as well as ongoing studies on the environmental tolerances of Oregon plants and animals, and experiments on the biological effects of global warming. As carbon dioxide levels increase, Oregon’s climate will move toward warm temperate, humid in the west and semiarid to subhumid to the east, with increased summer and winter drought in the west. Western Oregon lowlands will become less suitable for temperate fruits and nuts and Pinot Noir grapes, but its hills will remain a productive softwood forest resource. Improved pasture and winter wheat crops will become more widespread in eastern Oregon. Tsunamis and stronger storms will exacerbate marine erosion along the Oregon Coast, with significant damage to coastal properties and cultural resources
The mating-specific Gα interacts with a kinesin-14 and regulates pheromone-induced nuclear migration in budding yeast
As a budding yeast cell elongates toward its mating partner, cytoplasmic microtubules connect the nucleus to the cell cortex at the growth tip. The Kar3 kinesin-like motor protein is then thought to stimulate plus-end depolymerization of these microtubules, thus drawing the nucleus closer to the site where cell fusion and karyogamy will occur. Here, we show that pheromone stimulates a microtubule-independent interaction between Kar3 and the mating-specific Gα protein Gpa1 and that Gpa1 affects both microtubule orientation and cortical contact. The membrane localization of Gpa1 was found to polarize early in the mating response, at about the same time that the microtubules begin to attach to the incipient growth site. In the absence of Gpa1, microtubules lose contact with the cortex upon shrinking and Kar3 is improperly localized, suggesting that Gpa1 is a cortical anchor for Kar3. We infer that Gpa1 serves as a positional determinant for Kar3-bound microtubule plus ends during mating. © 2009 by The American Society for Cell Biology
Spatial Guilds in the Serengeti Food Web Revealed by a Bayesian Group Model
Food webs, networks of feeding relationships among organisms, provide
fundamental insights into mechanisms that determine ecosystem stability and
persistence. Despite long-standing interest in the compartmental structure of
food webs, past network analyses of food webs have been constrained by a
standard definition of compartments, or modules, that requires many links
within compartments and few links between them. Empirical analyses have been
further limited by low-resolution data for primary producers. In this paper, we
present a Bayesian computational method for identifying group structure in food
webs using a flexible definition of a group that can describe both functional
roles and standard compartments. The Serengeti ecosystem provides an
opportunity to examine structure in a newly compiled food web that includes
species-level resolution among plants, allowing us to address whether groups in
the food web correspond to tightly-connected compartments or functional groups,
and whether network structure reflects spatial or trophic organization, or a
combination of the two. We have compiled the major mammalian and plant
components of the Serengeti food web from published literature, and we infer
its group structure using our method. We find that network structure
corresponds to spatially distinct plant groups coupled at higher trophic levels
by groups of herbivores, which are in turn coupled by carnivore groups. Thus
the group structure of the Serengeti web represents a mixture of trophic guild
structure and spatial patterns, in contrast to the standard compartments
typically identified in ecological networks. From data consisting only of nodes
and links, the group structure that emerges supports recent ideas on spatial
coupling and energy channels in ecosystems that have been proposed as important
for persistence.Comment: 28 pages, 6 figures (+ 3 supporting), 2 tables (+ 4 supporting
Insufficient Production and Tissue Delivery of CD4+Memory T Cells in Rapidly Progressive Simian Immunodeficiency Virus Infection
The mechanisms linking human immunodeficiency virus replication to the progressive immunodeficiency of acquired immune deficiency syndrome are controversial, particularly the relative contribution of CD4+ T cell destruction. Here, we used the simian immunodeficiency virus (SIV) model to investigate the relationship between systemic CD4+ T cell dynamics and rapid disease progression. Of 18 rhesus macaques (RMs) infected with CCR5-tropic SIVmac239 (n = 14) or CXCR4-tropic SIVmac155T3 (n = 4), 4 of the former group manifested end-stage SIV disease by 200 d after infection. In SIVmac155T3 infections, naive CD4+ T cells were dramatically depleted, but this population was spared by SIVmac239, even in rapid progressors. In contrast, all SIVmac239-infected RMs demonstrated substantial systemic depletion of CD4+ memory T cells by day 28 after infection. Surprisingly, the extent of CD4+ memory T cell depletion was not, by itself, a strong predictor of rapid progression. However, in all RMs destined for stable infection, this depletion was countered by a striking increase in production of short-lived CD4+ memory T cells, many of which rapidly migrated to tissue. In all rapid progressors (P < 0.0001), production of these cells initiated but failed by day 42 of infection, and tissue delivery of new CD4+ memory T cells ceased. Thus, although profound depletion of tissue CD4+ memory T cells appeared to be a prerequisite for early pathogenesis, it was the inability to respond to this depletion with sustained production of tissue-homing CD4+ memory T cells that best distinguished rapid progressors, suggesting that mechanisms of the CD4+ memory T cell generation play a crucial role in maintaining immune homeostasis in stable SIV infection
Granulomatous hepatitis due to Bartonella henselae infection in an immunocompetent patient
<p>Abstract</p> <p>Background</p> <p><it>Bartonella henselae </it>(<it>B. henselae</it>) is considered a rare cause of granulomatous hepatitis. Due to the fastidious growth characteristics of the bacteria, the limited sensitivity of histopathological stains, and the non-specific histological findings on liver biopsy, the diagnosis of hepatic bartonellosis can be difficult to establish. Furthermore, the optimal treatment of established hepatic bartonellosis remains controversial.</p> <p>Case presentation</p> <p>We present a case of hepatic bartonellosis in an immunocompetent woman who presented with right upper quadrant pain and a five cm right hepatic lobe mass on CT scan. The patient underwent a right hepatic lobectomy. Surgical pathology revealed florid necrotizing granulomatous hepatitis, favoring an infectious etiology. Despite extensive histological and serological evaluation a definitive diagnosis was not established initially. Thirteen months after initial presentation, hepatic bartonellosis was diagnosed by PCR studies from surgically excised liver tissue. Interestingly, the hepatic granulomas persisted and <it>Bartonella henselae </it>was isolated from the patient's enriched blood culture after several courses of antibiotic therapy.</p> <p>Conclusion</p> <p>The diagnosis of hepatic bartonellosis is exceedingly difficult to establish and requires a high degree of clinical suspicion. Recently developed, PCR-based approaches may be required in select patients to make the diagnosis. The optimal antimicrobial therapy for hepatic bartonellosis has not been established, and close follow-up is needed to ensure successful eradication of the infection.</p
Ultraviolet Study of the Active Interacting Binary Star R Arae using Archival IUE Data
The eclipsing and strongly interacting binary star system R Arae (HD149730)
is in a very active and very short-lived stage of its evolution. R Ara consists
of a B9V primary and an unknown secondary. We have collected the International
Ultraviolet Explorer (IUE) archival data on R Ara, with most of the data being
studied for the first time. There are 117 high resolution IUE spectra taken in
1980, 1982, 1985, 1989, and 1991. We provide photometric and spectroscopic
evidence for mass transfer and propose a geometry for the accretion structure.
We use colour scale radial velocity plots to view the complicated behavior of
the blended absorption features and to distinguish the motions of hotter and
cooler regions within the system. We observed a primary eclipse of R Ara in
2008 and have verified that its period is increasing. A model of the system and
its evolutionary status is presented.Comment: 13 pages, 15 figures, accepted for publication in MNRA
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