Deep Time Conservation Paleobiology of the Atlantic Jigsaw Puzzle and the Future of the Southwestern Angolan Coast

L. Jacobs, M. Polcyn, O. Mateus, A. Schulp
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Abstract

The puzzle-like fit of Africa and South America reflects the tectonically driven opening of the South Atlantic Ocean beginning over 130 mya. By 90 Ma, the North and South Atlantics were conjoined. The introduction of Cretaceous marine reptiles into the central South Atlantic from the north coincides with through-flow in the Equatorial Atlantic Gateway and with increased productivity and upwelling of the Benguela Current. The K-Pg extinction saw the demise of most marine reptiles, but upwelling apparently persisted, evidenced by a growing Cenozoic fossil record of sea turtles and marine mammals from the Angolan coast. Convergent similarities between the Cretaceous marine reptile vertebrate community and the modern vertebrate community of the Benguela Large Marine Ecosystem suggest essentially continuous productivity related to upwelling along the southwest African coast since Cretaceous time. Paleolatitude reconstructions show that predicted positions of coastal upwelling of the Benguela Current have moved south along the coast as Africa drifted northward through the descending limb of the southern Hadley Cell. The Cretaceous and modern faunas were both adapted to a productive upwelling zone. The Cretaceous relict Welwitschia mirabilis is consistent with coastal aridity alongside upwelling. Thus, the sediments of coastal Angola and the fossils they entomb are relevant to conservation paleobiology because they provide a baseline through deep time. Comparisons underscore the resilience of the Benguela Current on the one hand and emphasize human-driven threats to the Benguela Large Marine Ecosystem on the other. Solutions are being sought; for instance, through the evaluation of Ecologically or Biologically Significant Marine Areas (EBSA) in the Benguela Current Large Marine Ecosystem. In Angola, the geologic record of the opening of the South Atlantic, the fossils, public interest, and the value for sustainable development are positive indications for the future.
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大西洋拼图的深时间保护古生物学和安哥拉西南海岸的未来
非洲和南美洲的拼图般的契合反映了1.3亿年前开始的构造驱动的南大西洋开放。到公元90年代,南北大西洋连在一起。白垩纪的海生爬行动物从北方进入南大西洋中部,与赤道大西洋门户的通流、生产力的提高和本格拉洋流的上涌不期而遇。K-Pg大灭绝见证了大多数海洋爬行动物的灭绝,但上升流显然持续存在,越来越多来自安哥拉海岸的新生代海龟和海洋哺乳动物化石记录证明了这一点。白垩纪海洋爬行类脊椎动物群落与本格拉大型海洋生态系统的现代脊椎动物群落之间的趋同相似性表明,自白垩纪以来,非洲西南海岸的上升流基本上是持续的生产力。古纬度重建显示,本格拉洋流的沿海上升流的预测位置已经沿着海岸向南移动,因为非洲通过南部哈德利单元的下降分支向北漂移。白垩纪和现代动物都适应了一个多产的上升流区。白垩纪遗存的奇异威氏藻与沿岸干旱区的上升流相一致。因此,安哥拉沿海的沉积物和它们埋葬的化石与保护古生物学有关,因为它们提供了深时间的基线。对比一方面强调了本格拉洋流的恢复力,另一方面强调了人为对本格拉大型海洋生态系统的威胁。正在寻求解决办法;例如,通过评估本格拉洋流大型海洋生态系统中具有生态或生物学意义的海洋区域(EBSA)。在安哥拉,南大西洋开放的地质记录、化石、公众利益和可持续发展的价值都是未来的积极迹象。
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