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Concept drift over geological times: predictive modeling baselines for analyzing the mammalian fossil record

机译:概念漂移在地质时代:预测模型基线,用于分析哺乳动物化石记录

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摘要

Fossils are the remains organisms from earlier geological periods preserved in sedimentary rock. The global fossil record documents and characterizes the evidence about organisms that existed at different times and places during the Earth's history. One of the major directions in computational analysis of such data is to reconstruct environmental conditions and track climate changes over millions of years. Distribution of fossil animals in space and time make informative features for such modeling, yet concept drift presents one of the main computational challenges. As species continuously go extinct and new species originate, animal communities today are different from the communities of the past, and the communities at different times in the past are different from each other. The fossil record is continuously increasing as new fossils and localities are being discovered, but it is not possible to observe or measure their environmental contexts directly, because the time is gone. Labeled data linking organisms to climate is available only for the present day, where climatic conditions can be measured. The approach is to train models on the present day and use them to predict climatic conditions over the past. But since species representation is continuously changing, transfer learning approaches are needed to make models applicable and climate estimates to be comparable across geological times. Here we discuss predictive modeling settings for such paleoclimate reconstruction from the fossil record. We compare and experimentally analyze three baseline approaches for predictive paleoclimate reconstruction: (1) averaging over habitats of species, (2) using presence-absence of species as features, and (3) using functional characteristics of species communities as features. Our experiments on the present day African data and a case study on the fossil data from the Turkana Basin over the last 7 million of years suggest that presence-absence approaches are the most accu
机译:化石是早期地质时期保存在沉积岩中的遗迹。全球化石记录文件并表征了关于在地球历史中不同时间和地区存在的有机体的证据。这些数据计算分析中的主要方向之一是重建环境条件,并跟踪气候变化超过数百万年。在空间和时间在空间和时间的分布使这种建模的信息特征成为一个主要的计算挑战之一。随着物种连续灭绝而新的物种起源,今天的动物社区与过去的社区不同,过去的不同时间的社区彼此不同。随着正在发现的新化石和地方,化石记录持续增加,但由于时间消失,不可能观察或衡量其环境范围。将有机体与气候相关的标记数据仅适用于当天可用,其中可以测量气候条件。该方法是在当天培训模型,并使用它们来预测过去的气候条件。但由于物种代表性不断变化,因此需要转移学习方法,以使模型适用和气候估计在地质时期可比较。在这里,我们讨论了从化石记录那种古古典重建的预测建模环境。我们比较并通过实验分析预测古气候重建的三种基线方法:(1)对物种的栖息地,(2)使用物种的存在,(3)使用物种社区的功能特征作为特征。我们对现今非洲数据的实验和对过去700万年里塔卡纳盆地的化石数据的案例研究表明,存在的缺勤方法是最大的ACCU

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