کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4463775 1621692 2011 9 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
High resolution δ18O and δ13C records from an annually laminated Scottish stalagmite and relationship with last millennium climate
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
High resolution δ18O and δ13C records from an annually laminated Scottish stalagmite and relationship with last millennium climate
چکیده انگلیسی

High-resolution (annual to decadal) stable isotope records of oxygen and carbon are analysed from an annually laminated stalagmite from NW Scotland. The sample, which was deposited for ~ 1000 yrs until 1996 AD, has previously provided annual resolution climate reconstructions of local rainfall and regional winter North Atlantic Oscillation (wNAO) from variations in annual growth rate. For our stalagmite, for which modern cave monitoring demonstrates that equilibrium deposition is highly likely for δ18O but not for δ13C, stalagmite δ13C originally derives from soil CO2 produced predominantly by microbial respiration, modified by degassing-related kinetic fractionation, and δ18O from the composition of infiltrating water during periods of infiltrating water. Both the presence of fluorescent laminae and modern drip-water monitoring demonstrate a drip hydrology that comprises both event and storage components. Over the instrumental period, no correlations between stalagmite or rainfall δ18O and precipitation amount or temperature are observed, but correlations are observed between rainfall δ18O and 500 mb height at regional IAEA monitoring stations. However, no correlations are observed between stalagmite δ18O and instrumental and reconstructed atmospheric circulation, preventing a simple palaeoclimate interpretation of the stalagmite δ18O proxy. Stalagmite δ13C has a stronger temporal autocorrelation than δ18O, indicative of soil mixing of respired CO2 and significant variability between drips and at different times; correlations with instrumental climate data are therefore not possible. The relative timing of changes in growth rate, δ18O and δ13C are discussed, and interpretations compared with other regional climate records. We conclude that, over the last millennium at this mid-latitude cave site, neither δ18O nor δ13C cannot be interpreted as a simple paleoclimate proxy.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Global and Planetary Change - Volume 79, Issues 3–4, December 2011, Pages 303–311
نویسندگان
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