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Author: WikiMatrix
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English[en]
The Ordovician and Silurian were warm greenhouse periods, with the highest sea levels of the Paleozoic (200 m above today's); the warm climate was interrupted only by a 30 million year cool period, the Early Palaeozoic Icehouse, culminating in the Hirnantian glaciation, 445 million years ago at the end of the Ordovician.
Indonesian[id]
Periode Ordovisium dan Silur merupakan periode “rumah kaca”, dengan permukaan air laut tertinggi dari Paleozoikum (200m lebih daripada hari ini); iklim hangat hanya disela oleh periode dingin selama 30 juta tahun, yakni Awal Paleozoikum Icehouse, yang berpuncak pada glasiasi Hirnantian.