Marine ecology

Worms start the reef-building process

Abstract

For reefs to form in wave-swept environments, the sessile organisms that build them need stable foundations1,2. Here we provide evidence that marine worms actively create patches of stable habitat on the sea bed which provide them with food and shelter. In so doing, they bring reef-building organisms together on hard surfaces and so create suitable conditions for reefs to develop.

Main

While maintaining a tropical marine aquarium, we noticed that three small colonies (each weighing 5–20 g) of the scleractinian reef coral Lobophyllia hemprichii on the tank's sandy bed had moved 6–16 cm during the night. The corals had become attached by a glue-like substance to a fist-sized lump of reef rock covered in coralline algae. Two colonies were stuck to the side of the rock about 2–4 cm above the sand bed.

We detached the corals from the reef rock and returned them to their former locations. The corals made night-time journeys to the reef rock 21 times over a 1-month period. A 90-degree alteration in the position of the reef rock with respect to the corals, or of the corals with respect to the reef rock, resulted in similar agglomeration around and affixation to the upper or lower sides of the rock.

We made several unsuccessful attempts to film this process under very weak background incandescent white or red light (less than 3 μmol photons m−2 s−1) and intermittent weak white or red light (1 minute on, 15 minutes off). Under constant background lighting, there was no movement of corals to the rock. During intermittent light–dark cycles, the corals moved on some occasions, but always during the dark period. This indicated that the corals were being moved rapidly by some photophobic agent.

We next mounted a Hi-8 video camera, equipped with infrared emission, perpendicular to the aquarium overnight. Less than 1 hour after darkness, the head and upper body of a bootlace-thick eunicid worm appeared from a hole in the rock. The worm sought out a coral and dragged it to the reef rock in less than 2 seconds (Fig. 1).

Figure 1: Patch reef construction by a eunicid worm in a reef aquarium.
figure1

Time-series images, captured from a video recording made under infrared illumination, of the rapid repositioning of a live scleractinian coral from sand bed to solid rock by a eunicid worm for the purposes of habitat assembly. The worm has been coloured to enhance visibility and the images have been adjusted using Adobe Photoshop to improve luminosity and contrast. The ruler in the background is graduated in centimetres and millimetres.

The persistent nightly efforts of the eunicid worm shown in Fig. 1 to expand and elaborate a durable habitat for itself suggest that such behaviour must have a genetic basis. Although immature, the worm shown in Fig. 1 could raise a 10-g piece of coral above the sand bed of the aquarium and cement it, with its photo-synthetic tissue orientated upwards, to the side of a piece of reef rock. Fully grown eunicid worms, which can be more than 2 m long3, must be able to assemble and bind together sizeable mounds of hard substrata.

The fossil record shows that the initial growth of coral reefs depends on the aggregation of sessile, skeleton-forming biota on a hard base1,2. It is not clear how these conditions arise on the shifting seafloors of continental shelf margins. Habitat construction by eunicid and related worms for protection and sustenance is a plausible explanation for both the patchy distribution of benthic communities in general and the development of coral reefs on otherwise unstable substrata1. By dragging together reef-building organisms and cementing them to mounds of hard substrata, they can assemble spatially heterogeneous, three-dimensional structures that trap sediments1, enhance settlement and growth of resident species4 and other reef biota1, and provide refuges for cryptic communities5,6.

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Correspondence to J. R. M. Chisholm.

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Chisholm, J., Kelley, R. Worms start the reef-building process. Nature 409, 152 (2001). https://doi.org/10.1038/35051660

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