Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.geoderma.2012.06.028 |
Meltwater seep patches increase heterogeneity of soil geochemistry and therefore habitat suitability | |
Ball, Becky A.1,2; Virginia, Ross A.2 | |
通讯作者 | Ball, Becky A. |
来源期刊 | GEODERMA
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ISSN | 0016-7061 |
EISSN | 1872-6259 |
出版年 | 2012 |
卷号 | 189页码:652-660 |
英文摘要 | The planet is undergoing an unequivocal period of climate change, with alterations in both longterm directional change and more local short-term variability. The amplified responses of polar ecosystems, and the potential feedbacks presented through alterations of soil processes, make it important to understand the consequences of climate change in polar soil systems. The McMurdo Dry Valleys of Antarctica have experienced periodic discrete warm climate events that result in melt water pulses from ice reserves, such as meltwater seep patches, alter geochemistry, and change habitat suitability for soil biotic communities and the ecological processes dictated by their activity. To investigate the consequences of soil seeps on soil geochemistry and biological activity, we sampled transects across six soil meltwater seep patches and measured soil water content, ion content, and potential CO2 flux to compare the seep habitat with the surrounding dry soil. We hypothesized that soils affected by meltwater seeps would be higher in salt content than the surrounding dry soils outside the seep patch. Though the increase in soil moisture in seeps could potentially increase biotic activity, we hypothesize that the osmotic stress resulting from a rise in soil salt concentration at the surface driven by evaporation would cause a decrease in biological activity. Our results show that seep patches increased soil moisture and salt content, particularly at the soil surface. The unaffected areas outside of seep patches differed widely in their ion content, typical of the high spatial geochemical heterogeneity found in the dry valleys. The presence of newly formed ice melt seeps can increase landscape-scale spatial heterogeneity by redistribution of soil salts from depth to the surface zone of the active layer. Seep patches have variable influence on biological activity, with both increases and decreases in respiration observed, related to the relative magnitudes of increases in moisture and salinity. (C) 2012 Elsevier B.V. All rights reserved. |
英文关键词 | Polar soils McMurdo Dry Valleys Ice melt Seeps Water pulse Desert soils |
类型 | Article |
语种 | 英语 |
国家 | USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000311875900072 |
WOS关键词 | MCMURDO DRY VALLEYS ; TAYLOR VALLEY ; COMMUNITY STRUCTURE ; ORGANIC-MATTER ; CLIMATE-CHANGE ; GLOBAL CHANGE ; BIODIVERSITY ; ECOSYSTEM ; DESERT ; LAKES |
WOS类目 | Soil Science |
WOS研究方向 | Agriculture |
来源机构 | Arizona State University ; Arizona State University |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/172523 |
作者单位 | 1.Arizona State Univ W Campus, Div Math & Nat Sci, Glendale, AZ 85306 USA; 2.Dartmouth Coll, Environm Studies Program, Hanover, NH 03755 USA |
推荐引用方式 GB/T 7714 | Ball, Becky A.,Virginia, Ross A.. Meltwater seep patches increase heterogeneity of soil geochemistry and therefore habitat suitability[J]. Arizona State University, Arizona State University,2012,189:652-660. |
APA | Ball, Becky A.,&Virginia, Ross A..(2012).Meltwater seep patches increase heterogeneity of soil geochemistry and therefore habitat suitability.GEODERMA,189,652-660. |
MLA | Ball, Becky A.,et al."Meltwater seep patches increase heterogeneity of soil geochemistry and therefore habitat suitability".GEODERMA 189(2012):652-660. |
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