A hundred years of Milutin Milankovic's climate change theory-geological implications

D. Radivojević
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Abstract

Milankovic?s cycles theory published hundred years ago is the most important theory in climate science and had great influence on Earth disciplines. Nevertheless, his work waited for more than fifty years for confirmation. It could be said that Milankovic?s work had most influence in creation of Astronomic Time Scale, supporting of continental drift hypothesis and palaeoclimatology implications. Positive results of the implementation of the astronomic time scale to the Neogene stratigraphy initiated the application of this method within the Mesozoic, and lately also to the Paleozoic sediments. Milankovic?s manuscript of astronomical forcing of climate changes led to fruitful cooperation with Alfred Wegener who was searching for additional arguments to validate his continental drift hypothesis. The factors that cause climate changes enable insight to the geological past, but also the possibility to model the climate conditions which await us in the future. Climate change prediction allowed people, as only being aware of its influence, to act preventively and take all measurements needed to reduce greenhouse gasses emission.
米卢廷·米兰科维奇的百年气候变化理论——地质意义
Milankovic吗?一百年前发表的地球周期理论是气候科学中最重要的理论,对地球学科产生了重大影响。然而,他的工作等了五十多年才得到证实。可以说,米兰科维奇?他的工作在天文时间尺度的建立、大陆漂移假说的支持和古气候学意义上影响最大。天文时间尺度应用于新近系地层的积极成果,开创了该方法在中生代的应用,近来也应用于古生代沉积物。Milankovic吗?他与阿尔弗雷德·韦格纳(Alfred Wegener)进行了卓有成效的合作,韦格纳当时正在寻找更多的论据来验证他的大陆漂移假说。导致气候变化的因素使我们能够洞悉过去的地质情况,也使我们有可能模拟未来等待我们的气候条件。气候变化预测使人们能够在意识到其影响的情况下采取预防行动,并采取一切必要措施减少温室气体排放。
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