Nitrogen subsidies in glacial meltwaters have altered planktonic diatom communities in lakes of the US Rocky Mountains for at least a century

Hydrobiologia ◽  
2017 ◽  
Vol 800 (1) ◽  
pp. 129-144 ◽  
Author(s):  
Krista E. H. Slemmons ◽  
Markie L. Rodgers ◽  
Jeffery R. Stone ◽  
Jasmine E. Saros
2013 ◽  
Vol 80 (3) ◽  
pp. 406-416 ◽  
Author(s):  
Vachel A. Carter ◽  
Andrea Brunelle ◽  
Thomas A. Minckley ◽  
Philip E. Dennison ◽  
Mitchell J. Power

Fire is one of the most important natural disturbances in the coniferous forests of the US Rocky Mountains. The Rocky Mountains are separated by a climatic boundary between 40° and 45° N, which we refer to as the central Rocky Mountains (CRM). To determine whether the fire regime from the CRM was more similar to the northern Rocky Mountains (NRM) or southern Rocky Mountains (SRM) during the Holocene, a 12,539-yr-old sediment core from Long Lake, Wyoming, located in the CRM was analyzed for charcoal and pollen. These data were then compared to charcoal records from the CRM, NRM and SRM. During the Younger Dryas chronozone, the fire regime was characterized as frequent at Long Lake. The early and middle Holocene fire regime was characterized as infrequent. A brief interval from 4000 to 3000 cal yr BP, termed the Populus period, had a frequent fire regime and remained frequent through the late Holocene at Long Lake. In comparison to sites from the NRM and SRM, the fire regime at Long Lake was most similar to the SRM during the past 12,539 cal yr BP. These results suggest the disturbance regime in the CRM has a greater affinity with those of the SRM.


2018 ◽  
Vol 221 (4) ◽  
pp. 1814-1830 ◽  
Author(s):  
Caelan Simeone ◽  
Marco P. Maneta ◽  
Zachary A. Holden ◽  
Gerard Sapes ◽  
Anna Sala ◽  
...  

2014 ◽  
Vol 34 (1) ◽  
pp. 34-43 ◽  
Author(s):  
Zaher Drira ◽  
Jannet Elloumi ◽  
Wassim Guermazi ◽  
Malika Bel Hassen ◽  
Asma Hamza ◽  
...  

2004 ◽  
Vol 82 (12) ◽  
pp. 1744-1757 ◽  
Author(s):  
Holger Cremer ◽  
Bernd Wagner

This contribution documents with light micrographs the planktonic diatom flora in seven high arctic lakes on Store Koldewey, an island off Northeast Greenland. The lakes have maximum water depths between 6.1 and 72.0 m. Basic limnological analyses indicate that all lakes are cold, monomictic, clear, oligotrophic, and alkaline. Planktonic diatoms and chrysophyte statospores were present in all but one lake. Eight planktonic diatom taxa were identified in the phytoplankton samples: Aulacoseira islandica (O. Müller) Simonsen, Aulacoseira tethera Haworth, Aulacoseira sp. 1, Cyclotella antiqua W. Smith, Cyclotella pseudostelligera Hustedt, Cyclotella rossii Håkansson, Fragilaria tenera (W. Smith) Lange-Bertalot, and Stephanodiscus minutulus (Kützing) Cleve et Möller. Fragilaria tenera was present in two morphotypes; the "normally shaped" type and a type with abnormally shaped valves, which has mostly been recorded in metal-polluted lakes. The diatom communities were generally dominated by only one or two species. The water columns of the lakes with a water depth greater than 10 m accomodate a moderate to high proportion of primarily benthic diatoms.Key words: Greenland, High Arctic, limnology, diatoms, valve morphology.


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