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Characterizing benthic substrates of Santa Monica Bay with seafloor photography and multibeam sonar imagery

机译:利用海底摄影和多束声纳图像表征圣莫尼卡湾底栖基质

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摘要

Seafloor photography from three cruises is combined with multibeam sonar imagery to characterize benthic substrates and associated fauna of Santa Monica Bay, California. The multibeam EM 1000 imagery was collected in 1996. Two sampling cruises (in 1998 and 1999) provided photographs at 142 sites throughout the Bay; a final cruise (in 2000) collected still photographs and continuous video along nine transects on the mainland shelf from Pt. Dume to the Palos Vcrdes peninsula. Muddy substrates (typically low backscatter) were the predominant habitat throughout the Santa Monica Bay, from the 20 m isobath to the adjacent Santa Monica basin floor (780 m). Bioturbation was pervasive as evidenced by abundant open burrows, mounds, and faunal tracks and trails. Sandy substrates (typically intermediate to high backscatter) were restricted to the innermost mainland shelf and a narrow outer shelf band north of Santa Monica Canyon. Cobble and gravel substrates (high backscatter) were restricted to the innermost shelf south of El Segundo and limited parts of the shelf edge. Rocky substrates (high backscatter) with interspersed patches of sand and gravel occurred on the high-relief marginal plateau and along parts of the shelf break offshore of Malibu.
机译:将三艘巡洋舰的海底摄影与多束声纳图像相结合,以表征底栖基质和加利福尼亚圣莫尼卡湾的相关动物群。多光束EM 1000影像是在1996年收集的。两次采样航行(分别在1998年和1999年)在整个海湾的142个地点提供了照片;最后一次巡游(2000年)是从Pt沿大陆架上的九个断面收集静止照片和连续视频。假装到帕洛斯Vcrdes半岛。从20 m等深线到相邻的Santa Monica盆地底部(780 m),整个圣莫尼卡湾的主要生境是泥泞的底物(通常是低反向散射)。生物扰动无处不在,如大量的空洞,土丘和动物群的踪迹所证明。沙质底物(通常在高反向散射的中间)仅限于圣莫尼卡峡谷以北的最内陆架和狭窄的外架带。卵石和砾石基质(高反向散射)仅限于El Segundo以南的最内层架子和架子边缘的有限部分。在浅浮雕边缘高原和沿马里布近海的部分陆架断裂上,出现了散布着沙子和砾石的岩石基质(高反向散射)。

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