Erin M. Dillon, D. McCauley, Brigida de Gracia, J. Cybulski, A. O’Dea
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在过去的半个世纪里,鲨鱼的数量有所下降,但变化的模式在不同的空间有所不同。鲨鱼数量的长期记录是有限的,这使得确定当地环境条件如何影响开发前鲨鱼基线及其对人类影响的易感性具有挑战性。我们使用保存在珊瑚礁沉积物中的鲨鱼鳞片(真皮小齿)来重建全新世中期和今天巴拿马地峡的鲨鱼群落。我们将这些数据与初级生产力、栖息地和鱼类丰度的记录一起解释,以探索每个海岸向更高营养水平的能量流。热带东太平洋是一个由季节性上升流驱动的生产系统,有着悠久的鲨鱼捕捞历史。另一方面,加勒比海岸是低营养和环境稳定的,采伐率较低。我们发现,犬齿积累率(鲨鱼丰度的代表)在太平洋巴拿马(巴拿马湾)比加勒比巴拿马(博卡斯德尔托罗)大一个数量级。巴拿马太平洋地区的初级生产力和鱼类丰度也较高,有助于支持这些大型捕食者种群。自全新世中期以来,巴拿马加勒比海地区的牙齿积累率下降了71%,其中包括远洋鲨鱼的选择性损失。相比之下,太平洋巴拿马的现代齿状体积累率与全新世中期的变化范围相当,并且齿状体组合的组成一直保持相似-这表明尽管密集捕捞,巴拿马湾的鲨鱼仍然存在。我们假设,该地区的高生产力可能是鲨鱼数量和明显恢复力的基础,因为捕食者的可用资源增加了。我们的发现揭示了能量在塑造鲨鱼基线的自然变化和恢复潜力方面的作用。他们还强调了将海洋学背景纳入鲨鱼管理的重要性。
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Reconstructing Millennial-Scale Variability in Reef Shark Communities Across The Isthmus of Panama
Shark populations have declined over the last half century, but the patterns of change vary across space. Long-term records of shark abundance are limited, making it challenging to determine how local environmental conditions influence pre-exploitation shark baselines and their susceptibility to human impacts. We use shark scales (dermal denticles) preserved in coral reef sediments to reconstruct shark communities during the mid-Holocene and today across the Isthmus of Panama. We interpret these data alongside records of primary productivity, habitat, and fish abundance to explore energy flow to higher trophic levels on each coast. The Tropical Eastern Pacific is a productive system driven by seasonal upwelling with a long history of shark exploitation. The Caribbean coast, on the other hand, is oligotrophic and environmentally stable, with lower rates of harvesting. We find that denticle accumulation rates, a proxy for shark abundance, are an order of magnitude greater in Pacific Panama (Gulf of Panama) than in Caribbean Panama (Bocas del Toro). Primary productivity and fish abundance are also higher in Pacific Panama, helping to support these large predator populations. Denticle accumulation rates declined by 71% since the mid-Holocene in Caribbean Panama, including a selective loss of pelagic sharks. In contrast, modern denticle accumulation rates in Pacific Panama are comparable to their range of variability during the mid-Holocene, and the composition of denticle assemblages remained similar through time—suggesting that sharks in the Gulf of Panama have persisted despite intensive fishing. We postulate that the region’s high productivity might underlie its high shark abundance and apparent resilience by increasing available resources for predators. Our findings shed light on the role of energy in shaping natural variability in shark baselines and recovery potential. They also highlight the importance of incorporating oceanographic context into shark management.
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