Effects of low pH and aluminum on amphibians at high elevation in the Sierra Nevada, California

1994 ◽  
Vol 72 (7) ◽  
pp. 1272-1279 ◽  
Author(s):  
David F. Bradford ◽  
Christina Swanson ◽  
Malcolm S. Gordon

At high elevation in the Sierra Nevada of California, surface waters are extremely low in acid-neutralizing capacity and thus may be vulnerable to changes in water chemistry due to acid deposition. The present study assesses the sensitivity of embryos and hatchling larvae of two Sierran amphibians, Pseudacris regilla (Pacific chorus frog) and Ambystoma macrodactylum (long-toed salamander), to low pH and an elevated level of dissolved aluminum. The populations of these two species are not known to be declining at present. These findings are compared with results for two other Sierran amphibians, Rana muscosa (mountain yellow-legged frog) and Bufo canorus (Yosemite toad), both of which reportedly have declined substantially in numbers in recent years. Embryos and hatchlings of P. regilla and A. macrodactylum were kept for 7 d in reconstituted soft water at pH 4.0–6.0 (inorganic monomeric aluminum effectively 0 or 39–80 μg/L at pH ≥ 4.9), and subsequently for a post-treatment period of up to 16 d in reconstituted soft water at pH 6.0 (no aluminum). LC50 pH values for post-treatment survival averaged 4.3 for embryos and tadpoles of both species. The estimated extreme pH for Sierra Nevada surface water, 5.0, did not cause a significant reduction in survival for either life stage of either species, and sublethal effects on body size and hatching time were not evident at pH ≥ 5.0. Aluminum also did not affect survival of either species, although sublethal effects were evident as reduced body size of A. macrodactylum larvae and earlier hatching in P. regilla. Pseudacris regilla and A. macrodactylum were not consistently more tolerant of low pH than R. muscosa and B. canorus. However, the latter two species show sublethal effects of low pH at pH ≥ 5.0, whereas the former two do not.

Analysis of sediment diatom and chrysophyte assemblages is the best technique currently available for inferring past lake water pH trends. Use of this approach for assessing the ecological effects of acidic deposition is increasing rapidly. As of August 1989, sediment core inferred pH data existed for at least 150 lakes in North America and cores from about 100 more lakes are being analysed. Equations for inferring past pH are based on at least 15-20 calibration data-sets involving about 700 lakes. Palaeolimnological studies indicate that recent acidification has been caused by acidic deposition in the Adirondack Mountains (New York), northern New England, Ontario, Quebec and the Canadian Atlantic provinces. Inferred pH decreases are commonly as much as 0.5-1.0 pH units. With the exception of one lake, no acidification trends were observed in regions currently receiving low deposition of strong acids (e.g. Rocky Mountains and Sierra Nevada in the western United States). Slight or no trends towards decreasing pH were observed in study lakes receiving moderately acidic deposition (upper Mid-west and northern Florida). The amount of inferred acidification (increase in H + concentration) correlates with the amount of S and N loading and the ability of watersheds and lakes to neutralize acid inputs, and is generally consistent with current lake-acidification theory. In most cases, the primary cause of recent acidification (post-1850) is acidic deposition, as opposed to land-use changes or natural processes, though these may be contributing factors. Acid loading has decreased in some regions since 1970 (e.g., northeastern United States). Some lakes have become less acidic in response, but others continue to lose acid neutralizing capacity. Many currently acidic lakes were naturally acidic (pH < 5.5) before the onset of anthropogenic acidification. These lakes are typically small (less than 10 ha) are located at moderately high elevations, have thin or peaty soils, or are located in outwash deposits. Many of these have acidified further recently.


2013 ◽  
Vol 50 (2) ◽  
pp. 159-174 ◽  
Author(s):  
James O. Sickman ◽  
Danuta M. Bennett ◽  
Delores M. Lucero ◽  
Thomas J. Whitmore ◽  
William F. Kenney

2016 ◽  
Vol 5 (04) ◽  
pp. 4524
Author(s):  
Abdullah Shaikh Farooque ◽  
Md. Azharuddin Ismail Atar*

Medicinal plants are being widely used, either as single drug or in combination in health care delivery system. Indian Sarsaparilla, Hemidesmus indicus (Family: Asclepiadaceae) is a commonly known Indian Medicinal Plant, which is widely recognized in traditional systems of Medicine. It contains various phytoconstituents belonging to the category glycosides, flavonoids, tannins, sterols and volatile oils. It has been reported as useful in biliousness, blood diseases, dysentery, diarrhea, respiratory disorders, skin diseases, syphilis, fever, leprosy, leucoderma, leucorrhoea, itching, bronchitis, asthma, eye diseases, epileptic fits in children, kidney and urinary disorders, loss of appetite, burning sensation, dyspepsia, nutritional disorders, ulcer and rheumatism. Several studies are being carried towards its activities like analgesic, anti-inflammatory, antiulcer, hepatoprotective, antioxidant and helicobactericidal properties. In our study we have evaluated antacid activity of sariva (Anantmool) by using In-Vitro method, i.e. ANC (Acid Neutralizing Capacity). This evaluation was done by comparing the ANC of sariva macerated & powdered drug with water as blank & standard drug i.e. NaHCO3. Based on this In-Vitro experiment, we can conclude that, the macerated & powdered drug of sariva (Anantmool) evaluated in this study, varied in potency as measured in terms of their ANC. These results having ** i.e. P < 0.01 & Passed the normality test. However, the present study being in-vitro, the effects of antacid may vary In-Vitro; individual variations also contribute to the ultimate effectiveness of as antacid.        


2007 ◽  
Vol 37 (12) ◽  
pp. 2508-2520 ◽  
Author(s):  
Constance I. Millar ◽  
Robert D. Westfall ◽  
Diane L. Delany

Limber pine ( Pinus flexilis James) stands along the eastern escarpment of the Sierra Nevada, California, experienced significant mortality from 1985 to 1995 during a period of sustained low precipitation and high temperature. The stands differ from old-growth limber pine forests in being dense, young, more even-aged, and located in warmer, drier microclimates. Tree growth showed high interannual variability. Relative to live trees, dead trees over their lifetimes had higher series sensitivity, grew more variably, and had lower growth. Although droughts recurred during the 20th century, tree mortality occurred only in the late 1980s. Significant correlations and interactions of growth and mortality dates with temperature and precipitation indicate that conditions of warmth plus sustained drought increased the likelihood of mortality in the 1985–1995 interval. This resembles a global-change-type drought, where warming combined with drought was an initial stress, trees were further weakened by dwarf mistletoe ( Arceuthobium cyanocarpum (A. Nels. ex Rydb.) A. Nels.), and proximally killed by mountain pine beetle ( Dendroctonus ponderosae Hopkins). However, the thinning effect of the drought-related mortality appears to have promoted resilience and improved near-term health of these stands, which suffered no additional mortality in the subsequent 1999–2004 drought.


Sign in / Sign up

Export Citation Format

Share Document