Downloaded from rsta.royalsocietypublishing.org on January 19, 2012 Long-period Milankovitch cycles from the Late Triassic and Early Jurassic of eastern North America and their implications for the calibration of the Early Mesozoic time−scale and the long −term behaviour of the planets Paul E. Olsen and Dennis V. Kent Phil. Trans. R. Soc. Lond. A 1999 357, 1761-1786 doi: 10.1098/rsta.1999.0400 Receive free email alerts when new articles cite this article - sign up in the box at the top right-hand Email alerting service corner of the article or click here To subscribe to Phil. Trans. R. Soc. Lond. A go to: http://rsta.royalsocietypublishing.org/subscriptions Downloaded from rsta.royalsocietypublishing.org on January 19, 2012 Long-period Milankovitch cycles from the Late Triassic and Early Jurassic of eastern North America and their implications for the calibration of the Early Mesozoic time-scale and the long-term behaviour of the planets By Paul E. Olsen1 and Dennis V. Kent2 1Lamont-Doherty Earth Observatory of Columbia University, Rt 9W, Palisades, NY 10964, USA (
[email protected]) 2Department of Geological Sciences, Rutgers University, Piscataway, NJ 08854, USA and Lamont-Doherty Earth Observatory of Columbia University, Rt 9W, Palisades, NY 10964, USA (
[email protected]) During the Late Triassic and Early Jurassic, the Newark rift basin of the northeastern US accumulated in excess of 5 km of continental, mostly lacustrine, strata that show a profound cyclicity caused by the astronomical forcing of tropical climate. The Newark record is known virtually in its entirety as a result of scientific and other coring and provides what is arguably one of the longest records of climate cyclicity available.