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Effects of elevated temperature on reproduction and larval settlement in Leptastrea purpurea 温度升高对紫纹细蛾繁殖及幼虫沉降的影响
Pub Date : 2022-03-27 DOI: 10.1007/s00338-022-02241-y
Nikko Galanto, C. Sartor, Victoria Moscato, Mykel Lizama, S. Lemer
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引用次数: 2
Living on the edge: environmental variability of a shallow late Holocene cold-water coral mound. 生活在边缘:全新世晚期浅层冷水珊瑚丘的环境变异性。
IF 3.5 Pub Date : 2022-01-01 Epub Date: 2022-04-12 DOI: 10.1007/s00338-022-02249-4
Jacek Raddatz, Volker Liebetrau, Andres Rüggeberg, Anneleen Foubert, Sascha Flögel, Dirk Nürnberg, Karen Hissmann, Johannes Musiol, Tyler Jay Goepfert, Anton Eisenhauer, Wolf-Christian Dullo

Similar to their tropical counterparts, cold-water corals (CWCs) are able to build large three-dimensional reef structures. These unique ecosystems are at risk due to ongoing climate change. In particular, ocean warming, ocean acidification and changes in the hydrological cycle may jeopardize the existence of CWCs. In order to predict how CWCs and their reefs or mounds will develop in the near future one important strategy is to study past fossil CWC mounds and especially shallow CWC ecosystems as they experience a greater environmental variability compared to other deep-water CWC ecosystems. We present results from a CWC mound off southern Norway. A sediment core drilled from this relatively shallow (~ 100 m) CWC mound exposes in full detail hydrographical changes during the late Holocene, which were crucial for mound build-up. We applied computed tomography, 230Th/U dating, and foraminiferal geochemical proxy reconstructions of bottom-water-temperature (Mg/Ca-based BWT), δ18O for seawater density, and the combination of both to infer salinity changes. Our results demonstrate that the CWC mound formed in the late Holocene between 4 kiloannum (ka) and 1.5 ka with an average aggradation rate of 104 cm/kiloyears (kyr), which is significantly lower than other Holocene Norwegian mounds. The reconstructed BWTMg/Ca and seawater density exhibit large variations throughout the entire period of mound formation, but are strikingly similar to modern in situ observations in the nearby Tisler Reef. We argue that BWT does not exert a primary control on CWC mound formation. Instead, strong salinity and seawater density variation throughout the entire mound sequence appears to be controlled by the interplay between the Atlantic Water (AW) inflow and the overlying, outflowing Baltic-Sea water. CWC growth and mound formation in the NE Skagerrak was supported by strong current flow, oxygen replenishment, the presence of a strong boundary layer and larval dispersal through the AW, but possibly inhibited by the influence of fresh Baltic Water during the late Holocene. Our study therefore highlights that modern shallow Norwegian CWC reefs may be particularly endangered due to changes in water-column stratification associated with increasing net precipitation caused by climate change.

Supplementary information: The online version contains supplementary material available at 10.1007/s00338-022-02249-4.

与热带珊瑚相似,冷水珊瑚(cwc)能够建造大型的三维珊瑚礁结构。由于持续的气候变化,这些独特的生态系统正处于危险之中。特别是,海洋变暖、海洋酸化和水文循环的变化可能危及cwc的存在。为了预测CWC及其珊瑚礁或丘在不久的将来将如何发展,一个重要的策略是研究过去的化石CWC丘,特别是浅层CWC生态系统,因为它们与其他深水CWC生态系统相比经历了更大的环境变异性。我们提出了来自挪威南部一个CWC丘的结果。从这个相对较浅(约100米)的CWC丘上钻取的沉积物岩心充分详细地揭示了全新世晚期的水文变化,这对丘的形成至关重要。应用计算机断层扫描、230Th/U定年、有孔虫地球化学代理重建底水温(Mg/Ca-based BWT)、海水密度δ18O,并结合两者推断盐度变化。研究结果表明,CWC丘形成于4 ~ 1.5 ka的全新世晚期,平均沉积速率为104 cm/千年(kyr),明显低于其他全新世挪威丘。重建的BWTMg/Ca和海水密度在整个土丘形成时期表现出很大的变化,但与附近Tisler Reef的现代原位观测结果惊人地相似。我们认为BWT对CWC丘的形成没有主要的控制作用。相反,整个土丘序列中强烈的盐度和海水密度变化似乎是由流入的大西洋水(AW)与上覆流出的波罗的海水之间的相互作用控制的。东北Skagerrak地区的CWC生长和小包形成受到强洋流、氧气补给、强边界层的存在和幼虫在海陆的扩散的支持,但可能受到全新世晚期波罗的海淡水的影响。因此,我们的研究强调,由于气候变化引起的净降水量增加,水柱分层的变化,现代挪威浅层CWC珊瑚礁可能特别濒危。补充信息:在线版本包含补充资料,下载地址:10.1007/s00338-022-02249-4。
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引用次数: 2
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Coral Reefs (Online)
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