Chemical constituents and IVDDM of hybrid cattail from a South Dakota prairie pothole

Wetlands ◽  
1988 ◽  
Vol 8 (2) ◽  
pp. 179-192 ◽  
Author(s):  
Daniel E. Hubbard ◽  
David A. Beck ◽  
Bryan D. Schultz
Wetlands ◽  
2009 ◽  
Vol 29 (2) ◽  
pp. 678-689 ◽  
Author(s):  
Sharon N. Kahara ◽  
Rachel M. Mockler ◽  
Kenneth F. Higgins ◽  
Steven R. Chipps ◽  
Rex R. Johnson

2004 ◽  
Vol 118 (2) ◽  
pp. 201 ◽  
Author(s):  
H. J. Homan ◽  
G. M. Linz ◽  
R. M. Engeman ◽  
L. B. Penry

Red-winged Blackbirds (Agelaius phoeniceus) are very abundant summer residents throughout the Prairie Pothole Region of central North America. In late summer they assemble in post-breeding flocks that cause significant amounts of agricultural damage, particularly in sunflower fields near natal sites. In April 2001, we aerially color-marked ~370,000 Red-winged Blackbirds near Badger, South Dakota (44°48'N, 97°21'W), to determine if migrants staging here were summer residents in sunflower production areas ~350 km to the northwest. We measured patterns of migratory dispersal by collecting birds in 54 randomly selected blocks in the northcentral U.S. and the Prairie Provinces of Canada. The marked specimens (n = 33) were categorized into three polygons based on analyses of banding and re-sighting data and proximity to concentrated sunflower production. We estimated that 82% of the migrants that had staged in eastern South Dakota resided within or on the periphery of the sunflower growing area. These birds probably stay near their breeding territories until at least late August and cause early damage to sunflower, which comprises the majority of damage. Resident birds in Alberta and most of Saskatchewan (18%) might arrive too late in the damage season to impact the sunflower crop significantly.


Wetlands ◽  
2001 ◽  
Vol 21 (1) ◽  
pp. 1-17 ◽  
Author(s):  
David E. Naugle ◽  
Rex R. Johnson ◽  
Michael E. Estey ◽  
Kenneth F. Higgins

Waterbirds ◽  
2013 ◽  
Vol 36 (3) ◽  
pp. 263-276 ◽  
Author(s):  
Neal D. Niemuth ◽  
Johann A. Walker ◽  
Jeffrey S. Gleason ◽  
Charles R. Loesch ◽  
Ronald E. Reynolds ◽  
...  

Wetlands ◽  
2000 ◽  
Vol 20 (4) ◽  
pp. 588-604 ◽  
Author(s):  
David E. Naugle ◽  
Rex R. Johnson ◽  
Michael E. Estey ◽  
Kenneth F. Higgins

2019 ◽  
Vol 11 (21) ◽  
pp. 2550 ◽  
Author(s):  
Woubet G. Alemu ◽  
Geoffrey M. Henebry ◽  
Assefa M. Melesse

Land surface phenologies and seasonalities in the US Prairie Pothole Region (PPR) were characterized using land surface variables derived from the coarse spatial resolution (25 km) Advanced Microwave Scanning Radiometer (AMSR) blended data for 2003 to 2016 linked with the optically based USDA NASS Crop Data Layer (CDL) at a much finer spatial resolution. Two transects of AMSR pixels—one in east-central North Dakota and the other in eastern South Dakota—were selected for analysis. The AMSR data were grouped earlier (2003–2005, 2007) and later (2013–2016) to emphasize temporal change and to avoid data discontinuity in 2011–2012 and a major drought in 2006. The nonparametric Mann-Kendall trend test on the CDL data revealed that area in grasslands and wetlands strongly decreased in both transects, while corn and soybean coverage strongly increased. In crop-dominated sites, the AMSR vegetation optical depth (VOD) time series caught the early spring growth, ploughing, and crop growth and senescence. In contrast, the VOD time series at grassland dominated sites exhibited a lower peak but extended growth period. Crop-dominated sites had significantly higher amplitude VODs in both periods and transects. Based on the paired two-sample t-test, neither the peak VOD amplitude nor the peak VOD timing measured in accumulated growing degree-days was significantly different between temporal groups in the North Dakota transect. In contrast, in South Dakota, both the peak VOD amplitude and its timing were significantly different with shifts to later peak timing during the 2013–2016 period. In addition, in South Dakota but not North Dakota, there were significantly earlier shifts in the timing of peak growing degree-days and peak precipitation water vapor. Both spatial and temporal changes in AMSR land surface variables are linked to shifts in land cover along the South Dakota transect as revealed in the CDL data. More research is required to understand the dynamics evident in the passive microwave time series.


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