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Using Stable Isotopes as Indicators, Tracers, and Recorders of Ecological Change: Some Context and Background

背景(考古学) 生态学 稳定同位素比值 环境变化 自然(考古学) 环境科学 地球科学 铅(地质) 生态系统 气候变化 地理 地质学 生物 古生物学 考古 物理 量子力学
作者
Todd E. Dawson,Rolf Siegwolf
标识
DOI:10.1016/s1936-7961(07)01001-9
摘要

The stable isotope investigations have grown steadily in the past 50 years or so and have become a cornerstone for many ecological investigations since the 1980s. The understanding of the many processes that lead to isotopic variation in natural environments is now often well understood and is improving each year. The challenge that is now being confronted with, is to extend what is known about these processes and the products that result from them, to see how changes have been ‘‘recorded’’ and how these changes can be interpreted. This requires a different approach that many past ecological investigations have not taken and one that forces ecologists to find materials such as carbonates, feathers, hard tissues, hair, tree-ring cellulose, and the many chemical compounds that compose them, so that they can be used to trace and therefore record change. By linking known processes to these changes, the growing field of ‘‘ecological forensics'’ that has emerged, is now documenting changes in many novel and powerful ways.Through innovative stable isotope methods and their novel application, the manner and magnitude of ecological transformations are now being documented across a wide range of natural systems. The environmental and ecological changes will continue and in many instances, will accelerate. Applying stable isotope analyses in these ways can lead to solutions that will help mitigate future ecosystem damage and environmental degradation.

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