Research Hub for Coral Reef Ecosystem Functions, James Cook University, Townsville, QLD 4811, Australia; College of Science and Engineering, James Cook University, Townsville, QLD 4811, Australia; ARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, QLD 4811, Australia.
Research Hub for Coral Reef Ecosystem Functions, James Cook University, Townsville, QLD 4811, Australia; College of Science and Engineering, James Cook University, Townsville, QLD 4811, Australia; ARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, QLD 4811, Australia.
Mar Pollut Bull. 2021 Aug;169:112580. doi: 10.1016/j.marpolbul.2021.112580. Epub 2021 Jun 5.
There is a rich literature on coral reef sediments. However, this knowledge is spread among research fields, and the extent to which major sediment reservoirs and reservoir connecting processes have been quantified is unclear. We examined the literature to quantify where and how sediments have been measured on coral reefs and, thereby, identified critical knowledge gaps. In most studies, sediments in one reservoir or one sedimentary process were quantified. The measurement of water column sediments (55% of reservoir measurements) and sediment trapping rates (42% of process measurements) were over-represented. In contrast, sediments on reef substrata, and the transition of sediments from the water column to the benthos, were rarely quantified. Furthermore, only ~20% of sediment measurements were accompanied by the quantification of hydrodynamic drivers. Multidisciplinary collaborative approaches offer great promise for advancing our understanding of the connections between sediment reservoirs, and the sedimentary and hydrodynamic processes that mediate these connections.
有关珊瑚礁沉积物的文献资料十分丰富。然而,这些知识分散在各个研究领域,主要沉积物储层和储层连接过程的量化程度尚不清楚。我们查阅了文献资料,以量化在珊瑚礁上测量沉积物的位置和方式,并确定了关键的知识空白。在大多数研究中,仅对一个储层或一个沉积过程中的沉积物进行了量化。对水柱沉积物(占储层测量的 55%)和沉积物捕获率(占过程测量的 42%)的测量过多。相比之下,对珊瑚礁基质上的沉积物以及水柱沉积物向海底转移的过程,却很少进行量化。此外,只有约 20%的沉积物测量值伴随着水动力驱动因素的量化。多学科合作方法为增进我们对沉积物储层之间的联系以及介导这些联系的沉积和水动力过程的理解提供了很大的希望。