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首页> 外文期刊>Journal of quaternary science: JQS >Tracing growing degree-day changes in the cuticle morphology of Betula nana leaves: A new micro-phenological palaeo-proxy
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Tracing growing degree-day changes in the cuticle morphology of Betula nana leaves: A new micro-phenological palaeo-proxy

机译:追踪西南桦叶片表皮形态的生长度-日变化:一种新的微观物候古代理

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摘要

Changing growing-season properties in the northern latitudes are among the most obvious consequences of ongoing global change. Available techniques including satellite monitoring and phenological observations enable the detection of changes over the last few decades to centuries, but the full range of natural variability is still difficult to capture. Here we introduce a new approach to reconstruct growing season properties, by studying imprints of prolonged growing season on epidermal cell growth in Betula nana. A high correlation between cell expansion determined in annually collected B. nana leaves and subfossil leaf fragments collected from recent peat sections in northern Scandinavia, and climatic indices such as budburst date, growing-season degree-days and May-September mean temperatures, enable the establishment of a new micro-phenological proxy for growing season characteristics. The applicability of the epidermal cell undulation index (UI) is tested by comparison with historical instrumental records of growing-season degree-days for the last 200 a. The results demonstrate the potential of the new leaf-morphology-based technique to reconstruct and quantify past changes in growing degree-days beyond instrumental data series. Applied to abundant B. nana leaf remains from peat and lake sediments, the UI may enable a reconstruction of growing degree-days throughout the Holocene and other parts of the late Quaternary.
机译:不断变化的北纬生长季节特性是正在进行的全球变化最明显的后果之一。包括卫星监测和物候观测在内的可用技术能够检测出过去几十年到几个世纪的变化,但是仍然很难捕获自然变化的全部范围。在这里,我们通过研究延长的生长季节对桦木(Betula nana)表皮细胞生长的影响,介绍了一种重构生长季节特性的新方法。斯堪的那维亚北部北部的每年泥炭地段每年收集的B. nana叶片和亚化石叶片碎片所确定的细胞膨胀与芽期,生长季节天数和5-9月平均温度等气候指数之间具有高度相关性。为生长季节特征建立新的微观物候代理。表皮细胞起伏指数(UI)的适用性是通过与过去200 a的生长季节天数的历史仪器记录进行比较来测试的。结果表明,基于新的基于叶形态学的技术有可能重建和量化超出仪器数据系列的生长日内过去的变化。将UI应用于泥炭和湖泊沉积物中大量的B. nana叶残留物,UI可以使整个全新世和第四纪晚期的其他部分的生长度日数得以重建。

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