scholarly journals Peer Review #2 of "Vascular plant biodiversity of the lower Coppermine River valley and vicinity (Nunavut, Canada): an annotated checklist of an Arctic flora (v0.1)"

2017 ◽  
Author(s):  
L Brouillet
Keyword(s):  
Peer Review ◽  
Vascular Plant ◽  
River Valley ◽  
Plant Biodiversity ◽  
Coppermine River ◽  
Annotated Checklist

scholarly journals Vascular plant biodiversity of the lower Coppermine River valley and vicinity (Nunavut, Canada): an annotated checklist of an Arctic flora

PeerJ ◽  
2017 ◽  
Vol 5 ◽  
pp. e2835 ◽  
Author(s):  
Jeffery M. Saarela ◽  
Paul C. Sokoloff ◽  
Roger D. Bull
Keyword(s):  
Sequence Data ◽  
Vascular Plant ◽  
River Valley ◽  
The Arctic ◽  
Polygonum Aviculare ◽  
Dna Sequence Data ◽  
Floristic Data ◽  
Coppermine River ◽  
Annotated Checklist ◽  
Made In

The Coppermine River in western Nunavut is one of Canada’s great Arctic rivers, yet its vascular plant flora is poorly known. Here, we report the results of a floristic inventory of the lower Coppermine River valley and vicinity, including Kugluk (Bloody Falls) Territorial Park and the hamlet of Kugluktuk. The study area is approximately 1,200 km2, extending from the forest-tundra south of the treeline to the Arctic coast. Vascular plant floristic data are based on a review of all previous collections from the area and more than 1,200 new collections made in 2014. Results are presented in an annotated checklist, including citation of all specimens examined, comments on taxonomy and distribution, and photographs for a subset of taxa. The vascular plant flora comprises 300 species (311 taxa), a 36.6% increase from the 190 species documented by previous collections made in the area over the last century, and is considerably more diverse than other local floras on mainland Nunavut. We document 207 taxa for Kugluk (Bloody Falls) Territorial Park, an important protected area for plants on mainland Nunavut. A total of 190 taxa are newly recorded for the study area. Of these, 14 taxa (13 species and one additional variety) are newly recorded for Nunavut (Allium schoenoprasum,Carex capitata,Draba lonchocarpa,Eremogone capillarissubsp.capillaris,Sabulina elegans,Eleocharis quinqueflora,Epilobiumcf.anagallidifolium,Botrychium neolunaria,Botrychium tunux,Festuca altaica,Polygonum aviculare,Salix ovalifoliavar.arctolitoralis,Salix ovalifoliavar.ovalifoliaandStuckenia pectinata), seven species are newly recorded for mainland Nunavut (Carex gynocrates,Carex livida,Cryptogramma stelleri,Draba simmonsii,Festuca viviparoideasubsp.viviparoidea,Juncus alpinoarticulatussubsp.americanusandSalix pseudomyrsinites) and 56 range extensions are reported. ThepsbA-trnHandrbcLDNA sequence data were used to help identify the threeBotrychiumtaxa recorded in the study area. Three new combinations are proposed:Petasites frigidussubsp.sagittatus(Banks ex Pursh) Saarela,Carex petricosasubsp.misandroides(Fernald) Saarela andCarex simpliciusculasubsp.subholarctica(T. V. Egorova) Saarela.

The late Wisconsinan olistostrome of the lower Coppermine River valley, Northwest Territories

1986 ◽  
Vol 23 (11) ◽  
pp. 1700-1708 ◽  
Author(s):  
Denis A. St-Onge ◽  
Jean Lajoie
Keyword(s):  
Debris Flows ◽  
Late Quaternary ◽  
Fine Sand ◽  
Coarse Sand ◽  
Coarse Fraction ◽  
River Valley ◽  
Glacial Lake ◽  
The North ◽  
Geologic Record ◽  
Coppermine River

The late Quaternary olistostrome exposed in the lower Coppermine River valley fills a paleovalley that ranges in apparent width from 150 to 400 m and was cut into Precambrian bedrock before the last glaciation. The olistostrome is here named the Sleigh Creek Formation. The coarse fraction of the formation is matrix supported; beds are massive or reversely graded and have sharp, nonerosive contacts. These characteristics suggest deposition of the coarse fraction by debris flows. The olistostrome sequence is bracketed by, and wedged into, a marine rhythmite sequence, which indicates that deposition occurred in a marine environment.About 10 500 years BP glacier ice in the Coronation Gulf lowland dammed the valley to the south, which was occupied by glacial Lake Coppermine. Sediments accumulated in this lake in a 30 m thick, coarsening upward sequence ranging from glaciolacustrine rhythmites of silt and fine sand at the base to coarse sand alluvium, and deltaic gravels at the top. As the Coronation Gulf lowlands became ice free, the Coppermine River reoccupied its former drainage course to the north. The steep south to north gradient and rapid downcutting by the river through the glacial lake sediments produced unstable slope conditions. The resulting debris flows filled a bedrock valley network below the postglacial sea level, forming the diamicton sequence.The interpretation of the Sleigh Creek Formation raises questions concerning silimar diamicton deposits usually defined as "flowtills." More generally, the results of this study indicate that care must be used when attempting paleogeographic reconstructions of "glaciogenic" deposits in marine sequences in any part of the geologic record.

scholarly journals Analysis of trophic structure of forest flora in the Oril River valley

2017 ◽  
Vol 18 (3-4) ◽  
pp. 37-50
Author(s):  
B. A. Baranovsky ◽  
I. A. Ivanko ◽  
A. V. Kotovych ◽  
L. A. Karmyzova ◽  
N. O. Roschina
Keyword(s):  
Plant Species ◽  
Forest Ecosystems ◽  
Black Locust ◽  
Vascular Plant ◽  
River Valley ◽  
Forest Vegetation ◽  
Current Status ◽  
Soil Conditions ◽  
Salix Alba ◽  
Common Oak

Biodiversity is important for maintaining of forest ecosystems functioning and in their resistance to anthropo-climatic challenges. Assessment of species diversity and species ecomorphic analysis is the basis for determining their current status, rational use and protection. At the end of the nineteenth century, Belgard A. L. (1950) in his system of ectomorphs using terminology presented by Dekandol (1956) and Warming (1903), had proposed a «trophomorph» category that reflected species relation to soil richness. Analysis of trophomorphs reflects diversity of soil conditions in different biotopes within forest ecosystems. The article gives an analysis on vascular plant trophomorphs distribution in various forest biotopes of Oril river valley. Flora and vegetation surveys in forests of Oril river valley were carried out by A. L. Belgard and T. F. Kirichenko since the 30s of the 20th century. The latest data on forest vegetation state within the Oril river valley were given in the works of Y. Gamulja and V. Manyuk. Generalized bioecological analysis of flora Oril river valley was represented in the monograph of B. Baranovsky, V. Maniuk, I. Ivanko, L. Karmyzova «Flora analysis of the Oril National Park». As is known, edaphic conditions of plant habitats in a first place are determined by soil fertility depending on the plant nutrients availability. Soddy-forest soil on sandy terrace of Oril river valley has a relatively low content of humus and total nitrogen: 2 and 0.04 %. Under these conditions, pine phytocenoses were ocсurred that represented exclusively by artificial plantings. Soils in the depressed area of Oril river floodplain are much richer in humus and nitrogen content (10 and 0.37 %). Here, arboreal and shrubby vegetation is represented by communities with common oak. On the second terrace of Oril river valley, forest vegetation is represented by artificial pine forests. Microcenoses with black locust, amorpha and willow occurred on elevated areas of sandy terrace (arena). In the depressed area of the arena, microcenoses with aspen and birch, aspen, Tatarian maple, amorpha, black locust were occurred additionally to pine communities. In the Oril floodplain, native arboreal and shrubby vegetation is represented mainly by communities with common oak. In depressed areas of the floodplain, microcenoses with white poplar, black poplar, aspen, Tatarian maple, amorpha, willow (Salix alba, S. fragilis), osiery (Salix cinerea, S. triandra),  and alder are fragmentarily occurred. In conditions of elevated areas of the floodplain, 196 vascular plants species were found, and 105 species in depressed areas. On the second terrace, 38 plant species grow on the elevated areas, and 54 species on the depressed ones. Flora includes 45 adventive plant species. In depressed floodplain areas, oligotrophs are represented by 7 species, mesotrophs by 126 species, megatrophs by 50 species, and in elevated areas: 7, 126 and 25 species, respectively. In depressed areas of arena oligotrophs are represented by 4 species, mesotrophs by 29 species, and megatrophs by 11, elevated areas: 7 and 21 species respectively, and megatrophs were absent.

scholarly journals Vascular Plant Diversity in Burned and Unburned Alvar Woodland: More Evidence of the Importance of Disturbance to Biodiversity and Conservation

2009 ◽  
Vol 123 (3) ◽  
pp. 240 ◽  
Author(s):  
Paul Catling
Keyword(s):  
Plant Diversity ◽  
Rare Species ◽  
Vegetation Cover ◽  
Vascular Plant ◽  
Plant Biodiversity ◽  
Vascular Plant Diversity ◽  
The Creation

Vascular plant biodiversity was compared in an unburned semi-open alvar woodland dominated by conifers and an equivalent woodland that had burned nine years previously and had developed into a long-lasting successional shrubland. The comparison, based on 30 quadrats 1 m2 at each of two sites, revealed less than 25% similarity in the vegetation cover of the two sites. The successional alvar shrubland that developed following fire had twice as many species and more regionally rare species than the corresponding woodland site. The shrubland also had higher values for various biodiversity measures that take heterogeneity and evenness into account. These data provide additional evidence for the importance of fire and disturbance in the creation of successional habitat upon which biodiversity depends. A cautious use of fire in management of alvars is supported.

scholarly journals Disentangling environmental correlates of vascular plant biodiversity in a Mediterranean hotspot

2013 ◽  
Vol 3 (14) ◽  
pp. 4849-4849
Author(s):  
Rafael Molina-Venegas ◽  
Abelardo Aparicio ◽  
Francisco José Pina ◽  
Benito Valdés ◽  
Juan Arroyo
Keyword(s):  
Vascular Plant ◽  
Plant Biodiversity ◽  
Environmental Correlates

Annotated checklist to the vascular plant flora of Tuktut Nogait National Park and the Melville Hills region (Canadian Low Arctic)

Phytotaxa ◽  
2013 ◽  
Vol 102 (1) ◽  
pp. 1 ◽  
Author(s):  
JEFFERY M. SAARELA ◽  
LYNN J. GILLESPIE ◽  
LAURIE L. CONSAUL ◽  
ROGER D. BULL
Keyword(s):  
Northwest Territories ◽  
National Park ◽  
Vascular Plant ◽  
Floristic Survey ◽  
Myriophyllum Sibiricum ◽  
Infraspecific Taxa ◽  
Plant Collections ◽  
Low Arctic ◽  
Conservation Concern ◽  
Annotated Checklist

 Tuktut Nogait National Park is located in the Melville Hills in the northeastern corner of mainland Northwest Territories in Canada's Southern Arctic Ecozone. The first major floristic survey of the Melville Hills region was conducted in 1990 as part of a natural resource inventory to determine its suitability as a National Park. We studied the flora and made extensive plant collections in Tuktut Nogait National Park and the Melville Hills region in 2009. Here, we present a comprehensive annotated checklist to the region's vascular plant flora based on a review of all existing and our own new collections. This includes the citation of all specimens examined, colour photographs for a subset of taxa and detailed taxonomic comments. The Melville Hills flora comprises 268 taxa (265 species and three additional infraspecific taxa), a 16% increase from the first survey, 215 of which are known from Tuktut Nogait National Park. Forty-eight taxa are newly recorded for the region and 54 taxa are newly recorded for Tuktut Nogait National Park. Noteworthy records include range extensions for Botrychium lunaria, Carex concinna, Draba borealis, Myriophyllum sibiricum, Plantago eriopoda, Poa alpina, Poa ammophila, Puccinellia banksiensis, Salix arbusculoides, and Selaginella selaginoides. The flora includes 19 vascular plant species of potential conservation concern in the Northwest Territories, including six assessed as "May Be At Risk", of which one occurs in the Park and 13 assessed as "Sensitive", of which eight occur in the Park.

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