Chamaesiphon komarekii species nova, a new benthic freshwater chroococcalean species (Cyanophyta/Cyanobacteria) from western coniferous forest streams in British Columbia, Canada

2008 ◽  
Vol 126 ◽  
pp. 37-46 ◽  
Author(s):  
Eugen Rott
2019 ◽  
Vol 56 (6) ◽  
pp. 688-692 ◽  
Author(s):  
Rolf W. Mathewes ◽  
Michael Richards ◽  
Thomas E. Reimchen

The basal portion of a fossil caribou antler from Graham Island is the only evidence of large terrestrial vertebrates older than the Fraser (late-Wisconsin) glaciation on Haida Gwaii. This antler has been radiocarbon dated three times by different laboratories and all ages fall within the mid-Wisconsin Olympia Interglaciation (Marine Isotope Stage 3, MIS 3). We suggest that the latest date, using ultrafiltration of bone collagen, is closest to the true age at 43 200 ± 650 years BP (48 200 – 45 200 cal BP). Previous paleoecological analysis from Graham Island reconstructed a vegetation cover during MIS 3 consisting of mixed coniferous forest with nonforested openings, similar to cool subalpine forests of today. These conditions are consistent with environments that support woodland caribou and the related extinct Dawson caribou. Morphometric comparison of antlers from woodland and Dawson caribou suggest that they are more similar than previously interpreted and raise questions about the inferred differences between the mainland and island subspecies.


1982 ◽  
Vol 60 (8) ◽  
pp. 1487-1494 ◽  
Author(s):  
Felix Bärlocher

Oak leaves and larch and spruce needles in fine-mesh (0.3 mm) and coarse-mesh (3 mm) bags were exposed in two hard-water streams in the Swiss Jura and two soft-water streams in the Black Forest. Periodically, conidium production in samples was determined under defined conditions. Generally, conidium production per unit weight was highest in oak, followed by larch and spruce. In oak and larch, an early peak was followed by a gradual decline; in spruce, conidium production reached an early plateau in the Jura streams but increased throughout the experimental period in the Black Forest streams. Percentage similarity between substrate spora and stream spora was highest for oak, followed by larch and spruce in three of the streams with deciduous riparian vegetation. The reverse sequence occurred in the remaining stream of a coniferous forest. On oak and larch, more fungal species were recovered in fine-mesh than in coarse-mesh bags; however, these additional species were numerically unimportant. Heliscus lugdunensis was the dominant species in early stages of spruce decay. It was replaced at later stages by Alatospora acuminata in the Jura streams and by two other species in the Black Forest streams. On oak and larch, the four or five most common species remained dominant throughout the experimental period.


1970 ◽  
Vol 48 (4) ◽  
pp. 779-788 ◽  
Author(s):  
John V. Matthews Jr.

A radiometrically dated Pliocene fossil locality in western Alaska contains specimens representing two new species of insects: Micropeplus hoogendorni n. sp. and Micropeplus hopkinsi n. sp. (Coleoptera: Staphylinidae, Micropeplinae). Fossils of the extant Micropeplinae species Kalissus nitidus LeConte and Micropeplus tesserula Curtis occur with the fossils of the newly described species. Other insect fossils and plant fossils from the locality suggest that M. hoogendorni and M. hopkinsi lived in a coniferous forest somewhat similar to those in present-day British Columbia or Southeastern Alaska.The holotype and paratypes of Micropeplus hopkinsi provide morphological evidence for the evolutionary sequence of elylral puncture development in the genus Micropeplus. This and other information is used to construct a provisional phylogeny for the subfamily Micropeplinae. The probable derivation of the species groups of Micropeplus is discussed.


1978 ◽  
Vol 100 (1) ◽  
pp. 64 ◽  
Author(s):  
N. H. Anderson ◽  
J. R. Sedell ◽  
L. M. Roberts ◽  
F. J. Triska

1978 ◽  
Vol 58 (1) ◽  
pp. 19-25 ◽  
Author(s):  
L. E. LOWE

Monosaccharide composition was determined on four major polysaccharide fractions of F and H horizons at three sites under different coniferous species. The major fractions studied were obtained by extraction with dilute acid (B), extraction with NaOH and fractionation of the fulvic fractions (FC), hydrolysis with 1 N H2SO4 (R1) and hydrolysis with 1 N H2SO4 after pretreatment with 72% H2SO4 (R2). Fraction R2 yielded virtually only glucose, and was assumed to represent cellulose, whereas the other fractions yielded six or more neutral sugars on hydrolysis. Marked differences in composition were observed between fractions B, FC and R1, particularly with respect to glucose and rhamnose contents and arabinose:xylose and mannose:galactose ratios. Horizon of origin had relatively less effect on fraction composition, with the exception of fraction B, for which the arabinose:xylose ratio decreased with increasing decomposition. Composition of fraction FC showed little variation between sites, whereas differences in composition of B and R1 fractions appeared to be associated with vegetation differences.


1970 ◽  
Vol 48 (7) ◽  
pp. 1383-1385 ◽  
Author(s):  
M. C. Kellman

The upper 10 cm of surface soil and litter beneath a coniferous forest in coastal British Columbia was found to contain over 1000 viable seeds per square meter. Alnus rubra Bong. made up 68.9% of all viable seed, although 18 other species, mainly weedy and secondary types, were recorded.


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