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Exceptionally well-preserved fossil specimens in the Fossil Basin of the Green River Formation (GRF) have made it the subject of extensive paleontological study, but the organic molecular framework that evolved during a key paleoclimatic and fossil-bearing interval during the early Eocene is poorly understood. 在绿河页岩（GRF）的化石盆地中， 保存异常完好的化石标本使其成为广泛古生物学研究的对象 ，但是在早始新世一个关键的古气候和含化石间隔期间发展起来的有机分子框架却了解甚少。 Whereas the organic geochemistry of the larger co-eval GRF basins has been extensively characterized, our molecular understanding of the fossil-bearing layers in the Fossil Basin and the drivers of the exceptional fossilization therein remain unresolved. 虽然已经广泛描述了较大GRF同期盆地的有机地球化学特征，但我们对化石盆地中含化石层的分子理解以及其中卓越化石保存的驱动因素仍
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