Dryas

基本解釋

Before the Younger Dryas, the world had been warming up as the last ice age came to an end.
在新仙女木期之前。由于冰河時期的結(jié)束，地球正在逐漸變暖。
Younger Dryas event (YD) is an abrupt cooling event in the warming period, a nearest and intense cooling event in the geologic record.
在目前持續(xù)升溫的情況下,研究YD事件的全球變化和區(qū)域響應(yīng)對了解未來氣候變化及其對自然環(huán)境和對人類社會的影響有著非常重要的意義。
But as for the cause of the Younger Dryas, the eyes of science were, until now, directed not up at the sky, but down into the ocean.
但在今天，以科學(xué)的眼光來看，新仙女木期的真正原因，并不是直接來自于天上，而是來自于海洋之中。
The variations of organic carbon, organic nitrogen, magnetic susceptibility and geochemi-cal element contents in core sediments all well coincide with the climatic change in the Dryas period.
巖心沉積物的有機(jī)碳、有機(jī)氮和磁化率以及化學(xué)元素含量的變化,都與仙女本期氣候變化具有十分吻合的變化態(tài)勢。
Palaeontologists have a name for the sudden cooling of the climate of the northern hemisphere that started right then and lasted for over a thousand years.They call it the Younger Dryas.
古生物學(xué)家將從那時開始并持續(xù)了超過一千年的北半球的氣候稱為新仙女木期。