Late Eocene to early Oligocene oxygen and carbon isotope records and biogenic...
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The late Eocene through early Oligocene (40-33 Ma) represents a transition from a warm-house to icehouse climate mode, with the expansion of Antarctic glaciation shortly after...
始新世晚期至渐新世早期(40~33 Ma,即4000万至3300万年前)是温室气候向冰室气候模式转变的过渡时期,此后不久南极冰盖便开始扩张……



