palaeolatitude
/ˌpælɪəʊˈlætɪtjuːd/( <美> paleolatitude)
noun
- the latitude of a place at some time in the past, measured relative to the earth's magnetic poles in the same period. Differences between this and the present latitude are caused by continental drift and movement of the earth's magnetic poles.古纬度（根据同时期磁极确定的纬度, 与现代纬度的差异是大陆漂移和地球磁极移动造成的）。