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The Effects of Cave Ventilation on Stalagmite Deposition and Paleoclimate Records--A Case Study from Cathedral Caverns, Alabama

机译:洞穴通风对石笋沉积和古气候记录的影响 - 以大教堂洞穴,阿拉巴马州的案例研究

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Speleothems (e.g., stalagmites) have been established as valuable archives of paleoclimate proxies (δ O_(carbonage) and δ C_(carbonate)). Studying stalagmites along the Gulf Coast has a high potential for producing paleo-rainfall records due to the abundance of carbonate (karst) in the region. In order to properly interpret these proxy records, the conditions within the cave in which the stalagmite was deposited must be well understood. Although the air temperature (-mean annual temperature) and relative humidity (~100%) of the atmosphere within caves are typically quite stable, recent studies have shown that slow density-driven movement of cave air can have profound seasonal changes in the chemistry of the cave air (pCO_2 and δ~(13)C), dripwater ([DIC], δ~(13)C_(DIC)), and the stalagmite (δ C~(13)C_(carbonate)). Furthermore, the primary season (e.g., winter) of stalagmite deposition can be controlled by this seemingly subtle process, which could have a profound influence on both the δ~(18)O and δ~(13)C chemistry preserved in the stalagmite. The measurement of pCO_2 throughout the year is the first step in determining cave ventilation and stagnation, because typically CO_2-rich cave air is diluted by CO_2-depleted atmospheric air during winter (ventilation mode). An on-going study since January 2015 at Cathedral Caverns (34°34'N, 86°13'W), located in northeastern Alabama, consists of the collection of air from the back of the cave (as well as ten other locations within the cave) near our stalagmite sample location. Preliminary results have shown a minimum and a maximum of 550 ppmV in February and 2820 ppmV in August, respectively, which indicates ventilation in winter (low pCO_2 values) and stagnation in summer (high pCO_2 values). These preliminary data indicate that a winter-bias of calcite deposition may be occurring and the interpretation of the paleo-record from Cathedral Caverns could be affected by such bias.
机译:已经建立了Speleothems(例如,石笋)作为古古古(δO_(碳造换)和δC_(碳酸盐))的有价值的档案。沿着海湾沿岸的石笋研究由于该地区的丰富碳酸盐(喀斯特)而产生古降雨记录的高潜力。为了正确解释这些代理记录,必须很好地理解沉积石笋的洞穴内的条件。虽然洞穴内的气氛( - emean年温)和相对湿度(〜100%)通常是相当稳定的,但最近的研究表明,洞穴空气的缓慢密度驱动的运动可能具有深刻的季节性变化洞穴空气(PCO_2和δ〜(13)C),滴水水([DIC],δ〜(13)C_(DIC))和石笋(δC〜(13)C_(碳酸盐))。此外,石笋沉积的主要季节(例如,冬季)可以通过这种看似微妙的过程来控制,这可能对δ〜(18)o和δ〜(13)C化学保存在石笋中的δ〜(18)和δ〜(13)的影响。全年的PCO_2的测量是确定洞穴通气和停滞的第一步,因为通常在冬季(通风模式)在CO_2耗尽的大气空气中稀释CO_2富含CO_2的洞穴空气。自2015年1月在大教堂洞穴(34°34'NN,86°13'W)以来,位于阿拉巴马州东北部的一项正在进行的研究,包括从洞穴的背面收集空气(以及内部的十个其他地方洞穴)附近我们的Stalagmite样本位置。初步结果分别显示了2月和2820分PPMV的最低和最多550 ppmv,分别在冬季(夏季低PCO_2值)和停滞状态(高PCO_2值)的通风。这些初步数据表明,可以发生方解石沉积的冬季偏差,并且来自大教堂洞穴的古纪录的解释可能受到这种偏差的影响。

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