首页> 外文期刊>Arctic: Journal of the Arctic Institute of North America >Pollen, oxygen isotope content and seasonality in an ice core from the Penny Ice Cap, Baffin Island
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Pollen, oxygen isotope content and seasonality in an ice core from the Penny Ice Cap, Baffin Island

机译:巴芬岛潘妮冰帽的冰芯中的花粉,氧同位素含量和季节性

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The results of pollen analyses of 12 ice core samples, covering an eight-year period from 1972 through 1979 from the divide of the Penny Ice Cap, Baffin Island, are reported. The pollen spectra are dominated by long distance transported pollen, especially the conifers Picea and Pinus. Alnus pollen is generally rare. In contrast, pollen spectra from both modern polsters and fossil peat sections in the same area are both characterized by local pollen types. Pollen influx values range from 2 to 8 grains/cm2/yr. Where the sampling intervals happened to coincide with established seasonal intervals (as interpreted from later oxygen isotope studies) the pollen spectra showed seasonal characteristics. This occurred in five out of the twelve samples. Comparison of these data is made with data from Devon Island Ice Cap. Such information may be useful in reconstructing paleoclimates.
机译:据报道,从巴芬岛潘妮冰帽的划分来看,从1972年到1979年的8年期间,对12个冰芯样品的花粉分析结果得到了报告。花粉光谱以长距离传播的花粉为主,尤其是针叶树Picea和Pinus。 nu花粉通常很少见。相比之下,同一地区的现代民粉和化石泥炭剖面的花粉光谱都具有局部花粉类型的特征。花粉流入值范围为2至8粒/ cm2 / yr。如果采样间隔恰好与确定的季节间隔一致(从后来的氧同位素研究中解释),则花粉光谱显示出季节特征。这发生在十二个样本中的五个样本中。这些数据与来自德文岛冰帽的数据进行了比较。这样的信息对于重建古气候可能是有用的。

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