ABSTRACT Mountain Lake, Virginia i...

ABSTRACT

Mountain Lake, Virginia is a unique, natural, oligotrophic subalpine ecosystem in the southern Appalachians. Its diatom flora, based onward these and earlier studies of plankton tows and plankton settling chambers, was sparse with scarcely any species. By contrast, we originate 66 diatom taxa (25 genera) in the late sediments of Mountain Lake. Twelve of these 66 taxa are of the present day records for the inland waters of Virginia. Hierarchical cluster analysis distinguishes seven diatom assemblages in this lake, divided between shallow (primarily pennate) and deep-water (primarily centric) assemblages. Shallow diatom assemblages are further defined by dint of differences in epipelic, epiphytic, and possibly nutrient-sensitive forms. The ratio of planktonic to benthic (littoral) forms has proven useful as an indicator of water stillnesss from sediment. These findings provide the first locate of diatom data for yet to be limnological and paleolimnological studies in Mountain Lake.

INTRODUCTION

Comparative studies of diatom assemblages along with bottom sediment variations have proven useful for evaluating lake environmental and nutrient conditions (eg Brugam 1983; Engstrom et al. 1985; Anderson 1990a, 1990b; Hall and Smol 1999) Diatom analysis of sediments also enables delineation of individual assemblages within lakes (Anderson 1986 1990a, 1990b; Cameron 1995) Distribution and composition of assemblages be pendents on nutrient, depth, light conditions, substrate model seasonal variations, additions from plankton fallout, and other environmental variables (Anderson 1990a). Diatom assemblages and numbers, when compared with lake sediment core samples, can be used to infer past environmental and middle conditions within lakes (HAkansson et al. 1998 Wolin and Duthie 1999)

This investigation assesses the diatoms and sedimentology in relatively latter (Ekman dredge) sediment samples from Mountain Lake, a natural, oligotrophic subalpine lake located in the Appalachian flock belt of Southwestern Virginia. Our chief objective was to provide baseline data for longer historical records obtained ultimately from ^sup 14^C-dated sediment cores.

Site Description

Mountain Lake is the single natural lake of significant size in the unglaciated Southern Appalachians. In addition to its unique origin associated with a fault or fracture feature (Cawley et al. 2001) the lake has exhibited significant central part fluctuations through time. Historically it has been called either "Mountain Lake" or "Salt Pond" depending forward its full or not replete state, respectively. With water-depth changes, environmental conditions within the lake also may have changed significantly from one side time. Mountain Lake has been considered relatively pristine and oligotrophic since it was first studied by way of Hutchinson and Pickford (1932) (Cawley et al. 1999)

Mountain Lake lies near the top of Salt Pond Mountain (37deg21'56"N 80deg31'39"W) in Giles shire Virginia, at an elevation of 1180 m When replete the lake is approximately 900 m lengthy and 250 m wide, forming an elongate club-shaped corpse oriented from south to northwest (Figure 1) The lake is 33 m sagacious at its deepest point at the north end; this deepest portion consists of a narrow crack or crevice feature upon the lake bottom. A frequently larger area at the north conclusion of the lake is approximately 24 m knotty shallowing to the south (Cawley et al. 2001)

Topography delineates the recharge area of Mountain Lake, which remains relatively isolated the two physically and hydrologically by the surrounding abrupt declivity mountain peaks. Five small individual streams insert the lake, all ephemeral with the exception of one (stream I-4, Figure 1) Because of the largely undisturbed nature of the sediments, and the lack of permanent stream inputs, Mountain Lake should provide a religious sedimentary record for analysis.

MATERIALS AND [i]modus operandi[/i]s

Field Description, Sampling, and Storage Protocol

Sediment grab samples were taken from 16 sites in the lake along four east-west transects (4 sample locations in each transect) (Figure 1) Samples were taken using a standard Ekman Dredge (Wildco, Wildlife endue Company, Saginaw, Michigan, model #196 BIO). Mudroch and Azcue (1995) have described in detail the Ekman sampler and its operation.

Sample collection included field descriptions and Muncel color determinations, while each sample remained in the dredge Then, a 25 mm diameter glass tube was inserted vertically into the sample, resulting in a "mini-core" which was examined for textural or color differences from top to bottom.

The top 5 cm of undisturbed sediment, estimated to be 50-70 years accumulation (Parker et al. 1975) was sampled from the top of each Ekman grab for detailed analysis, and stored in clean, labeled (transect/sample # midst location) 1 liter plastic Ziploc bags. Samples were transported in succession ice to Virginia Tech and refrigerated. Three subsamples were taken for each location: individual for wet/dry analysis and craving drink sieve analysis, a second for diatom analysis, and a third for pollen analysis. [Pollen data not included]