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Miocene flooding events of western Amazonia

机译:西亚马逊地区的中新世洪水事件

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There is a considerable controversy about whether western Amazonia was ever covered by marine waters during the Miocene [23 to 5 Ma (million years ago)]. We investigated the possible occurrence of Miocene marine incursions in the Llanos and Amazonas/Solim?es basins, using sedimentological and palynological data from two sediment cores taken in eastern Colombia and northwestern Brazil together with seismic information. We observed two distinct marine intervals in the Llanos Basin, an early Miocene that lasted ~0.9 My (million years) (18.1 to 17.2 Ma) and a middle Miocene that lasted ~3.7 My (16.1 to 12.4 Ma). These two marine intervals are also seen in Amazonas/Solim?es Basin (northwestern Amazonia) but were much shorter in duration, ~0.2 My (18.0 to 17.8 Ma) and ~0.4 My (14.1 to 13.7 Ma), respectively. Our results indicate that shallow marine waters covered the region at least twice during the Miocene, but the events were short-lived, rather than a continuous full-marine occupancy of Amazonian landscape over millions of years.
机译:关于中新世[23至5Ma(百万年前)]期间,亚马逊河西部是否曾被海水覆盖,存在着很大的争议。我们使用哥伦比亚东部和巴西西北部两个沉积岩心的沉积学和孢粉学数据以及地震信息,调查了拉诺斯岛和亚马孙州/ Solim?es盆地中新世海侵的可能发生。我们在拉诺斯盆地观察到两个不同的海相间隔,一个持续了约0.9 My(百万年)(18.1至17.2 Ma)的中新世中期和持续了约3.7 My(16.1至12.4 Ma)的一个中新世。这两个海相间隔也见于亚马逊河/ Solim?es盆地(西北亚马逊地区),但持续时间短得多,分别为〜0.2 My(18.0至17.8 Ma)和〜0.4 My(14.1至13.7 Ma)。我们的结果表明,在中新世期间,浅海海水至少覆盖了该区域两次,但这些事件是短暂的,而不是数百万年以来海洋生物对海洋景观的持续占用。

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