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胡安·费尔南德斯群岛钾氩测年的植物学和地质学意义。

Botanical and geological significance of potassium-argon dates from the juan fernandez islands.

出版信息

Science. 1984 Jul 6;225(4657):49-51. doi: 10.1126/science.225.4657.49.

Abstract

Potassium-argon dating of five basalts from the three main islands of the Juan Fernández (or Robinson Crusoe) Islands of Chile in the southeastern Pacific gives ages of 1.01 +/- 0.12 and 2.44 +/- 0.14 million years for Masafuera, 3.79 +/- 0.20 and 4.23 +/- 0.16 for Masatierra, and 5.8 +/- 2.1 for Santa Clara. These ages are much younger than that of the underlying oceanic plate and are consistent with the origin of the island-seamount chain from a mantle hot spot beneath the eastward moving Nazca plate. The young age for the archipelago suggests that speciation within endemic genera has occurred within the past 4 to 5 million years. Endemic genera of apparently more ancient origins, such as Lactoris and Thyrsopteris, have apparently dispersed to the islands and survive refugially.

摘要

对智利东南太平洋胡安·费尔南德斯群岛(或鲁滨逊·克鲁索岛)三个主要岛屿的五块玄武岩进行钾-氩定年,结果显示马萨富埃拉年龄为 1.01 +/- 0.12 和 2.44 +/- 0.14 百万年,马萨蒂埃拉年龄为 3.79 +/- 0.20 和 4.23 +/- 0.16 百万年,圣克拉拉年龄为 5.8 +/- 2.1 百万年。这些年龄远小于基底洋壳的年龄,与岛屿-海山链起源于向东移动的纳斯卡板块下方地幔热点的观点一致。该群岛的年轻年龄表明,特有属内的物种形成发生在过去的 400 万至 500 万年。起源明显更古老的特有属,如 Lactoris 和 Thyrsopteris,显然已扩散到这些岛屿,并在避难所中幸存下来。

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