Distribution, production, and diversity of C3- and C4-dominated communities in a mixed prairie

1983 ◽  
Vol 61 (3) ◽  
pp. 741-751 ◽  
Author(s):  
Paul W. Barnes ◽  
Larry L. Tieszen ◽  
David J. Ode

The vegetation composition and standing crop of 44 stands, representing a diversity of topographic sites, were examined in a Northern Great Plains mixed prairie to determine the distribution, diversity, and relative production of different C3 and C4 dominated plant communities. Cluster analysis identified seven species groups at the 40% similarity level; these have been identified as seven community types: high prairie, midprairie, low prairie, meadow, depression, mud flats, and marsh. Environmental variables which showed the highest significant correlation with the three axes of a modified Bray and Curtis indirect ordination were soil moisture regime, soil potassium, and soil nitrate. Analysis of δ13C biomass values indicate that the greatest abundance (nearly 50%) of C4 biomass occurs in low prairie with roughly one-third of meadow and high prairie biomass contributed by C4 species. C4 biomass contribution appears greatest on soils relatively low to moderate in nitrate, potassium, phosphorous, and moisture, yet C4 species cooccur with C3 species where these resources are low. Both productivity and species diversity are related to topographic features but productivity does not appear to be functionally determined by the relative proportion or contribution of C4 taxa. The greatest number of C4 species occupy upland slopes and ridges and within these habitats C3 and C4 grasses may be distributed differently depending on slope exposure.


1993 ◽  
Vol 73 (4) ◽  
pp. 765-778 ◽  
Author(s):  
W. D. Willms ◽  
P. G. Jefferson

The mixed prairie represents the most arid region of the Northern Great Plains in Canada. Approximately 6.5 M ha of the original total of 24 M ha have retained their native character. The native prairie supports about 5.3 M animal–unit–months or about 15% of all beef cattle present on the Canadian prairies. A large portion of the area is dominated by either needle-and-thread (Stipa comata Trin. + Rupr.) or western wheatgrass (Agropyron smithii Rydb.), both cool season grasses, and associated with blue grama [Bouteloua gracilis (H.B.K.) Lag. ex Steud.] a warm season grass. These species define the major plant communities of the mixed prairie and determine their production potential. However, their production is limited by available water during the growing season and by soil nutrients; factors which also influence their species composition. Grazing imposes a significant impact on the grasslands by altering the water and nutrient cycles, through defoliation and reduced plant litter, and eventually by affecting the species composition. Removing litter may reduce forage production by up to 60% and repeated defoliation will favour the more drought tolerant but less productive species. Forage production may be increased by seeding introduced species, which have a greater shoot to root ratio than native grasses, or with fertilizer application. Livestock production may be increased with the use of grazing systems. However, the benefits of each practice on the mixed prairie must be assessed in terms of their cost, their impact on the environment, and the reduced or lost value for other users. Key words: Biomass, above-ground, below-ground, water-use efficiency, reseeding, soil fertility, grazing efficiency



2018 ◽  
Vol 57 (2) ◽  
pp. 319-331 ◽  
Author(s):  
David Changnon

AbstractHeavy 30-day snowfall amounts were evaluated to identify spatial and temporal characteristics east of the Rocky Mountains in the United States during the period 1900–2016. An extensive data assessment identified 507 stations for use in this long-term climate study. The top 30-day heavy snowfall amount and the average of the top five 30-day heavy snowfall amounts were examined. Both amounts generally increased with latitude; however, much higher amounts were found downwind of the Great Lakes, at higher elevations, or in locations impacted by topographic features (e.g., Rockies, Black Hills, and Appalachians). When compared with the 1981–2010 average winter snowfall, the top 30-day amount was found to be greater than the winter average in most areas of the eastern United States. The number of stations experiencing a top-five 30-day heavy snowfall period in a winter ranged from 1 to 128 (1959/60), with a greater overall occurrence in the second half of the 117-yr period. Six episodes had 10% or more stations experiencing one of the top five 30-day snowfall amounts, with the February–March 1960 episode impacting 124 stations, and these episodes were associated with large negative 500-hPa height anomalies. The northern Great Plains, Great Lakes, Midwest, and Northeast experienced more top-five periods in the second half of the 117-yr period, whereas most of the southern states experienced top-five periods throughout the study’s time frame. Examining extremes at periods beyond the daily event and less than the season contributes to our knowledge of climate and provides useful information to snow-sensitive sectors.





1977 ◽  
Author(s):  
R.C. Severson ◽  
L.P. Gough ◽  
J.M. McNeal


2007 ◽  
Vol 99 (4) ◽  
pp. 904-911 ◽  
Author(s):  
D. L. Tanaka ◽  
J. M. Krupinsky ◽  
S. D. Merrill ◽  
M. A. Liebig ◽  
J. D. Hanson


2002 ◽  
Vol 66 (1) ◽  
pp. 202 ◽  
Author(s):  
M. Tejedor ◽  
C. C. Jiménez ◽  
F. Díaz


2020 ◽  
Vol 0 (0) ◽  
pp. 0-0
Author(s):  
Shimaa Hassan ◽  
Salah AbdEl-kareem ◽  
Samia Massoud ◽  
Mohamed Abdallah


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