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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >BayMBT: A Bayesian calibration model for branched glycerol dialkyl glycerol tetraethers in soils and peats
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BayMBT: A Bayesian calibration model for branched glycerol dialkyl glycerol tetraethers in soils and peats

机译:BayMBT:用于土壤和泥炭的支链甘油二烷基甘油甘油四乙酯的贝叶斯校准模型

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Accurate temperature records for the deep geological past are a vital component of paleoclimate research. Distributional changes of branched glycerol dialkyl glycerol tetraether (brGDGT) lipids in geological archives including paleosoils are a promising indicators to infer past continental air temperatures. However, the 'orphan' status of the brGDGTs, the potential effect of temperature-independent parameters on their relative distribution, and the uneven geographical distribution of the soils used for calibration contribute to the high uncertainty of brGDGT-based transfer functions (root mean squared error, RMSE: +/- 5 degrees C). Here, we expand the soil dataset from the previous calibration(s) with new and published soil data. We use Bayesian statistics to calibrate the relationship of the 5-methyl brGDGTs (MBT'(5Me)) and mean annual air temperature (MAAT). The addition of soils from warm (>28 degrees C) environments from India substantially increases the upper limit of the Bayesian calibration (BayMBT) from 25 to 29 degrees C, aiding in the generation of temperature records for past greenhouse climates, such as the Eocene. The BayMBT model also effectively minimizes the structured MAAT residuals prevalent in previous calibrations, therefore giving the opportunity to explore confounding factors on the calibration. We formulate a set of alternative calibration models to test the effect of specific environmental parameters and show that soils at mid-latitudes with temperature seasonalities >20 degrees C are not well described by the BayMBT model. We find that the MBT'(5)(Me) index is best correlated to the average temperature of all months >0 degrees C, called the BayMBT(0) model. This finding supports the hypothesis that brGDGT production ceases or slows down in the winter months. However, a persistent feature of the BayMBT model and previous calibrations is the significant scatter at mid-latitudes, which is speculatively linked with a possible increase in diversity of microbial brGDGT-producing communities in these locations. (C) 2019 The Author(s). Published by Elsevier Ltd.
机译:深层地质过去的准确温度记录是古古基强行研究的重要组成部分。在包括古盘子的地质档案中分布甘油二烷基甘油四醚(BRGDGT)脂质的分配变化是推断过大陆空气温度的有望指标。但是,BRGDGTS的“孤儿”状态,温度无关的参数对其相对分布的潜在影响,以及用于校准的土壤的不均匀地理分布有助于BRGDGT的转移函数的高不确定性(根均方错误,RMSE:+/- 5℃)。在这里,我们将土壤数据集与新的和公布的土壤数据扩展到先前的校准。我们使用贝叶斯统计来校准5-甲基BRGDGTS(MBT'(5ME))和平均年度气温(MAAT)的关系。从印度的温暖(> 28摄氏度)环境中的土壤增加了25至29摄氏度的贝叶斯校准(BayMBT)的上限,同时在过去温室气候的温度记录中的产生中,例如eocene 。 BayMBT模型还有效地减少了先前校准中普遍存在的结构化的Maat残差,因此有机会在校准中探索混淆因素。我们制定了一组替代校准模型,以测试特定环境参数的效果,并表明八国集型模型中的温度季节性和温度季节性态度下游的土壤。我们发现,MBT'(5)(ME)指数与称为BayMBT(0)模型的所有月份> 0摄氏度的平均温度最佳。这一发现支持BRGDGT生产在冬季停止或减慢的假设。然而,BayMBT模型和先前校准的持续特征是中纬度地区的显着散射,其猜测性地与这些位置中的微生物BRGDGT的多样性的可能增加。 (c)2019年作者。 elsevier有限公司出版

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