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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >Late Quaternary climate change in the Awatere Valley, South Island, New Zealand using a sine model with a maximum likelihood envelope on fossil beetle data
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Late Quaternary climate change in the Awatere Valley, South Island, New Zealand using a sine model with a maximum likelihood envelope on fossil beetle data

机译:使用正弦模型在化石甲虫数据上使用最大似然包络线,在新西兰南岛的阿沃特河谷晚第四纪气候变化中

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We present a new climatic reconstruction method appropriate for biological proxies where modern distributions are poorly defined and data sets are small. The technique uses a sine function in conjunction with maximum likelihood estimates of best high and best low values for the distribution of each species. To demonstrate the model we present temperature reconstructions for the Last Glacial Maximum (LGM) and Holocene from beetle fossil assemblages from the Awatere Valley, New Zealand. The temperature estimates are determined by the mutual overlap of the climate range for all the species in the assemblage. The overlap is then compared with modern physio-chemical conditions.For our example, we estimate the LGM summer (February) mean temperature was about 3.5-4degreesC cooler, and July (winter) mean daily minimum temperature was about 4-5degreesC cooler than present day temperatures. The maximum likelihood estimates broaden the reconstructed temperature ranges to 2.5-5degreesC cooler for February temperatures and 3.5-6.0degreesC cooler for mean minimum daily temperature of the coldest month (July). These estimates are consistent with LGM temperature estimates of 4-7degreesC from other climate proxy indicators.Estimates of Holocene temperatures are very similar to modern. Estimates are compared with results from the established mutual climatic range (MCR) technique and the results are compatible. MCR is less robust than the sine model approach for these data because it requires the pre-determination of the critical physiochemical controls and assumes Gaussian distributions in climate space. The sine model is conceptually superior to traditional BIOCLIM modelling, with which it shares many features, because BIOCLIM also assumes Gaussian distributions and the sine model allows attribute testing of the data sets which are not possible with BIOCLIM. (C) 2004 Elsevier Ltd. All rights reserved.
机译:我们提出了一种新的气候重建方法,适用于现代分布定义不清且数据集较小的生物代理。该技术将正弦函数与每个物种分布的最佳高值和最佳低值的最大似然估计结合使用。为了演示该模型,我们介绍了来自新西兰Awatere谷地的甲虫化石组合的最后冰期最大值(LGM)和全新世的温度重建。温度估计值取决于组合中所有物种的气候范围相互重叠。然后将重叠部分与现代理化条件进行比较。在我们的示例中,我们估计LGM夏季(2月)的平均温度大约低3.5-4°C,7月(冬季)的每日最低温度比现在低4-5°C一天的温度。最大似然估计将重建的温度范围扩大到2月温度较凉爽的2.5-5°C和最冷月份(7月)的平均最低每日温度凉爽的3.5-6.0°C。这些估计值与其他气候代用指标的LGM温度估计值4-7°C一致。全新世温度的估计与现代温度非常相似。将估计值与已建立的共同气候范围(MCR)技术的结果进行比较,结果是兼容的。对于这些数据,MCR不如正弦模型方法强健,因为它需要对关键的理化控制进行预先确定,并假设气候空间呈高斯分布。正弦模型在概念上优于传统的BIOCLIM建模,后者具有许多功能,因为BIOCLIM还假定高斯分布,并且正弦模型允许对数据集进行属性测试,而BIOCLIM则无法进行。 (C)2004 Elsevier Ltd.保留所有权利。

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