The chemokine,CXCL16, and its receptor,CXCR6, are constitutively expressed in human annulus fibrosus and expression of CXCL16 is up-regulated by exposure to IL-1ß in vitro

Chemokines are an important group of soluble molecules with specialized functions in inflammation. The roles of many specialized chemokines and their receptors remain poorly understood in the human intervertebral disc. We investigated CXCL16 and its receptor, CXCR6, to determine their immunolocalization in disc tissue and their presence following exposure of cultured human annulus fibrosus cells to proinflammatory cytokines. CXCL16 is a marker for inflammation; it also can induce hypoxia-inducible factor 1α (HIF-1α), which is a phenotypic marker of heathy nucleus pulposus tissue. We found CXCL16 and CXCR6 immunostaining in many cells of the annulus portion of the disc. Molecular studies showed that annulus fibrosus cells exposed to IL-1ß, but not TNF-α, exhibited significant up-regulation of CXCL16 expression vs. control cells. There was no significant difference in the percentage of annulus cells that exhibited immunolocalization of CXCL16 in grade I/II, grade III or grade IV/V specimens. The presence of CXCL16 and its receptor, CXCR6, in the annulus in vivo suggests the need for future research concerning the role of this chemokine in proinflammatory functions, HIF-1α expression and disc vascularization.     

Early devonian flora of the trout valley formation of northern maine

The data on the plant fossils of the Trout Valley Formation of north-central Maine, U.S.A., are summarized. Evidence from lithological correlation, from plant megafossils and paleopalynology suggest a late Early Devonian (Emsian) age for the Formation. Plant megafossils present are several species of Psilophyton, Pertica quadrifaria, Kaulangiophyton akantha, Prototaxites sp., Drepanophycus sp., Taeniocrada sp. and Thursophyton sp. The microfossil assemblage, through poorly preserved, contains Deltoidospora sp., Apiculiretusispora sp., Emphanisporites rotatus, E. annulatus, Clivosisporites cf. C. verrucata, Grandispora sp. and a chitinozoan, Sphaerochitina sp. The ancient landscape is suggested as having been an area a few square miles in extent with modest relief and comparable to a modern brackish or fresh-water marsh. Three other floras, one in Maine, a second in New Brunswick, Canada, and a third along the coast of Gaspé Bay, Quebec, are thought to have been at least partially contemporaneous with the Trout Valley flora.     

Chemotaxonomy of some problematic palaeozoic plants

Chemical data are given on the remains of nine fossil genera ranging from Precambrian to Carboniferous in age (Chuaria, Sporangites, Taeniocrada, Orestovia, Parka, Protosalvinia, Spongiophyton, Solenites, Botryococcus). It is suggested that such chemical data are useful additional criteria in making taxonomic assignments in palaeontology. Analyses indicate a high level of organic chemical diversity, although the original composition has evidently been altered by temperature and pressure over a long period of time. The labile chemical constituents are retained within a more chemically inert carbon matrix, which shows a progressive alteration of the ratios of C, N, O and H with respect relative age, similar to that seen in the coalification process.The chemical composition of Sporangites specimens is more suggestive of an animal rather than a plant affinity; it is here suggested that this genus represents in part the remains of some animal egg test. Hydrolytic products of Solenites and Taeniocrada indicate the presence of aliphatic hydroxy acids suggesting the presence of cutin and suberin. The chemical compositions of Orestovia, Parka, Protosalvinia, Spongiophyton and Botryococcus are interpreted as being consistent with an algal rather than a vascular plant affinity. Evidence for extreme diagenesis of the acritarch-like Chuaria greatly limits chemotaxonomic consideration. The possible role of thermal and biotic-thermal degradation patterns seen in palaeochemistry is discussed.     

Stomatal Density Responses of Egyptian Olea europaea L. Leaves to CO2 Change Since 1327 BC

We have attempted to separate the effects of CO₂ and temperaturechange on stomatal density by examining ancient leaf materialof Olea europaea L. The distribution of this species is confinedto a Mediterranean type climate, so that O. europaea leavesof different ages will have formed under similar temperaturesbut different CO₂ levels over the last 3000 years. Stomataldensity measurements have been made upon leaves of O. europaeaoriginating from King Tutankhamun's tomb dating from 1327 BC,and have been compared with values obtained from Egyptian O.europaea material dating from pre-332 BC, 1818 and 1978 AD.Together, the four dates provide a record of how the plant hasresponded to increases in atmospheric CO₂ concentration duringthat time. The results demonstrate that in accordance with similarstudies examining the stomatal density response of plants overthree time scales (hundreds, thousands and tens of thousandsof years) stomatal density falls as CO₂ levels increase. Sincewe have examined a natural system with leaves developing undersimilar environmental temperatures the results confirm observationsfrom experimental studies in which plants were grown under thesame temperature but different CO₂ regimes.Copyright 1993, 1999Academic Press Olea europaea, stomatal density, atmospheric CO₂, temperature, climate change     

Dynamics of Dual Infection with Campylobacter jejuni Strains in Chickens Reveals Distinct Strain-to-Strain Variation in Infection Ecology

Although multiple genotypes of Campylobacter jejuni may be isolated from the same commercial broiler flock, little is known about the infection dynamics of different genotypes within individuals or their colonization sites within the gut. Single experimental infections with C. jejuni M1 (sequence type 137, clonal complex 45) and C. jejuni 13126 (sequence type 21, clonal complex 21) revealed that 13126 colonized the ceca at significantly higher levels. The dissemination and colonization sites of the two C. jejuni strains then were examined in an experimental broiler flock. Two 33-day-old broiler chickens were infected with M1 and two with 13126, and 15 birds were left unchallenged. Cloacal swabs were taken postinfection to determine the colonization and shedding of each strain. By 2 days postinfection (dpi), 8/19 birds were shedding M1 whereas none were shedding 13126. At 8 dpi, all birds were shedding both strains. At 18 dpi, liver and cecal levels of each isolate were quantified, while in 10 birds they also were quantified at nine sites throughout the gastrointestinal (GI) tract. 13126 was found throughout the GI tract, while M1 was largely restricted to the ceca and colon. The livers of 7/19 birds were culture positive for 13126 only. These data show that 13126 has a distinctly different infection biology than strain M1. It showed slower colonization of the lower GI tract but was more invasive and able to colonize at a high level throughout the GI tract. The finding that C. jejuni strains have markedly different infection ecologies within the chicken has implications for control in the poultry industry and suggests that the contamination risk of edible tissues is dependent on the isolate involved.     

Stomatal Density and Index of Fossil Plants Track Atmospheric Carbon Dioxide in the Palaeozoic

It has been demonstrated that the leaves of a range of foresttree species have responded to the rising concentration of atmosphericCO₂ over the last 200 years by a decrease in both stomatal densityand stomatal index. This response has also been demonstratedexperimentally by growing plants under elevated CO₂ concentrations.Investigation of Quaternary fossil leaves has shown a correspondingstomatal response to changing CO₂ concentrations through a glacial-interglacialcycle, as revealed by ice core data. Tertiary leaves show asimilar pattern of stomatal density change, using palynologicalevidence of palaeo-temperature as a proxy measure of CO₂ concentration.The present work extends this approach into the Palaeozoic fossilplant record. The stomatal density and index of Early Devonian,Carboniferous and Early Permian plants has been investigated,to test for any relationship that they may show with the changesin atmospheric CO₂ concentration, derived from physical evidence,over that period. Observed changes in the stomatal data givesupport to the suggestion from physical evidence, that atmosphericCO₂ concentrations fell from an Early Devonian high of 10-12times its present value, to one comparable to that of the presentday by the end of the Carboniferous. These results suggest thatstomatal density of fossil leaves has potential value for assessingchanges in atmospheric CO₂ concentration through geologicaltime.Copyright 1995, 1999 Academic Press Aglaophyton major, Sawdonia ornata, Swillingtonia denticulata, Lebachia frondosa, Juncus effusus, Psilotum nudum, Araucaria heterophylla, stomatal density, stomatal index, Palaeozoic CO₂     

The Impact of Atmospheric CO2 and Temperature Changes on Stomatal Density: Observation from Quercus robur Lammas Leaves

A comparative study of leaves formed on shoots during the springand summer (lammas) of Quercus robur from three contrastinggeographical locations (Cardiff, Durham and London) gives ameasure of the effect of temperature on stomatal density. Thisis of value in attempting to distinguish the effects of CO₂and temperature on observed stomatal density changes under differentCO₂ and temperature conditions through the Quaternary. Theseleaves of normal and lammas shoots will have developed undersimilar CO₂ levels but different environmental temperatures.Our results demonstrate that leaves formed under the warmersummer temperatures had reduced stomatal densities and indicesfrom all sites, compared with their spring counterparts. Thistrend was also detected from measurements of spring and summerleaves made upon herbarium material collected from the sametree in 1840. The results suggest that for Q. robur temperatureoverrides the influence of irradiance intensity and small seasonal(