Abstract
Mesophotic coral ecosystems (MCEs), which comprise the light-dependent communities of corals and other organisms found at depths between 30 and ~150 m, have become a topic that increasingly draws the attention of coral reef researchers. It is well established that after the reef-building scleractinian corals, octocorals are the second most common group of macrobenthic animals on many shallow Indo-Pacific reefs. This chapter reviews the existing knowledge (e.g., species composition and depth of occurrence) on octocorals from selected Indo-Pacific MCEs: Okinawa (Japan), Palau, South Africa, the northern Red Sea, and the Great Barrier Reef (Australia). For all reefs, zooxanthellate taxa are not found below 65 m. We, therefore, suggest that physiological constraints of their symbiotic algae limit the depth distribution of zooxanthellate octocorals. More studies of lower MCEs (60–150 m) and their transition to deepwater communities are needed to answer questions regarding the taxonomy, evolutionary origins, and phylogenetic uniqueness of these mesophotic octocorals. New findings on mesophotic octocoral sexual reproduction indicate a temporal reproductive isolation between shallow and mesophotic octocoral populations, thus challenging the possibility of connectivity between the two populations. The existing data should encourage future studies aimed at a greater understanding of the spatiotemporal features and ecological role of mesophotic octocorals in reef ecosystems.
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Notes
- 1.
Samples were collected by ROV (ECA H800) operated from the R/V Sam Rothberg. In situ photography used a low-light black and white camera VS300 (Eca Robotics) and 1CAM Alpha HD camera (SubCimaging). Octocoral samples were collected using a manipulator arm on the ROV, and fragments of colonies were carefully preserved in 100% ethanol for molecular work. The original samples were placed in 70% ethanol for taxonomic identification and deposited at the Steinhardt Museum of Natural History, Israel National Center for Biodiversity Studies.
- 2.
The AUV collected geo-referenced, stereo images with a footprint of 1.5 × 1.2 m at a rate of ~1 image pair every 50 cm. We randomly selected 30 images separated by at least 2 m (to avoid double counting from image overlap) from within 6 depth bins (10–20, 20–30, 30–40, 40–50, 50–60, and 60–70 m) representing shallow to mesophotic depths. Images were further divided into “seaward” and “leeward” aspects, depending upon their location. The GBR outer shelf supports long, linear lines of submerged shoals along the shelf edge with tops at ~15 m water depth (Hopley et al. 2007), and these features are common at Hydrographers Passage (Beaman et al. 2011). In this study, “leeward” aspect sites were considered as those occurring on the leeside of these shoals, while “seaward” aspect sites were those on the seaward side. Not all depth bins contained enough images to fulfill all the selection criteria, although each aspect/depth combination contained at least 22 images for analysis.
Each image was visually inspected for soft corals, and the abundance of each genus is recorded using scale of relative abundance (sensu DeVantier et al. 1998). Relative abundance of each genus was scored as 1, 1–10% cover; 2, 11–30%; 3, 31–50%; 4, 51–75%; and 5, 76–100%. Taxonomic identifications based on images were informed by specimens collected from the same region concomitantly with the AUV surveys. In addition, very small colonies (<10 cm in diameter) were excluded from our analysis. Changes in community composition were assessed using multivariate techniques in PRIMER V6 (Clarke and Gorley 2006). Analyses were performed on an untransformed Bray-Curtis similarity matrix, and the relationship between images in all aspect/depth combinations was visualized using principal coordinates analysis (PCO), with Spearman rank correlation vectors showing the relationship between the dominant taxa and sites.
- 3.
During the breeding season, colonies were monitored almost daily underwater in marked 30 × 1 m belt transects in both depth zones. Each day, when encountered, the number of R. f. fulvum colonies with surface-brooded embryos or planulae was recorded and their percentage of the total number of colonies was calculated.
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Acknowledgments
We thank the Interuniversity Institute for Marine Sciences in Eilat for the use of the R/V Sam Rothberg and the professional assistance of its crew members. We are indebted to EcoOcean staff members for operating the ROV. Special thanks are due to L.P. van Ofwegen, Naturalis Biodiversity Center, Leiden, The Netherlands, for his support and help in taxonomy. We acknowledge A. Gonzalez for laboratory assistance, A. Shlagman for curatorial skills, V. Wexler for digital editing, and N. Paz for editorial assistance. Special thanks are due to K. Fabricius for identifying the GBR octocorals. Collection efforts in Palau were supported by the US National Cancer Institute with identification made by P. Alderslade and L.P. van Ofwegen. Special thanks go to CRRF staff Lori Bell Colin, Matt Mesubed, and Emilio Basilius.
This research was supported in part by the TASCMAR project (tools and strategies to access original bioactive compounds from cultivated marine invertebrates and associated symbionts) that has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No. 634674 and the Israel Cohen Chair in Environmental Zoology to YB. Collection of animals complied with official permits issued by the respective authorities.
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Benayahu, Y. et al. (2019). Octocorals of the Indo-Pacific. In: Loya, Y., Puglise, K., Bridge, T. (eds) Mesophotic Coral Ecosystems. Coral Reefs of the World, vol 12. Springer, Cham. https://doi.org/10.1007/978-3-319-92735-0_38
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