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MESOPHOTIC CORAL ECOSYSTEMS – A LIFEBOAT FOR CORAL REEFS?

16

ucture

acclimatization strategies (both ecological and biological).

These include the following (reviewed in Kahng et al. 2010,

2014):

• Minimizing self-shading and maximizing surface area at

a colony morphology level (e.g. horizontally flattened or

encrusting colony morphologies), at a cellular level (e.g.

monolayered zooxanthellate), and possibly at a subcellular

level.

• Reducing the amount of tissue biomass, surface area and

respiratory demand to increase growth efficiency.

• Reducing skeletal mass per unit colony area to reduce

energy requirements.

• Optimizing skeletal light-scattering properties (Figure

2.10).

The reflective properties of calcium carbonate play an

important role in increasing the light-harvesting efficiency of

mesophotic corals (Enríquez et al. 2005, Kahng et al. 2012a,

Kahng 2014) and may also occur in other organisms, such

as calcareous green algae and coralline red algae. For a plant

leaf (or non-calcareous macroalgae), light passes through the

tissue only once and, unless absorbed by pigments, is lost. In

contrast, the skeleton of a coral can reflect light back through

the tissue, thereby increasing the probability of absorption.

Light-harvesting efficiency is not only influenced by skeletal

composition, but can also be affected by the light-scattering

properties of skeletal micromorphology. Internal scattering

can increase the probability of light absorption, independent of

pigment concentration, by increasing the photon path length

within the coral tissue (Figure 2.10).

Location can also affect the amount of ambient light available

for mesophotic corals and algae. On flat or gently sloping

areas, sessile organisms can be exposed to diffuse low light

throughout the day, but on a steep slope, light is limited

because the slope obstructs the light for a portion of the day

(Brakel 1979). Thus, an MCE in clear water may have ample

light at a given depth in areas with flat open seafloor, but may

Figure 2.11.

A near-vertical mesophotic reef slope on thewestern

side of Tobi (Hatohobei) Island, Palau at 55 m in depth. This area

is heavily shaded during morning periods when the sun is in the

east, casting a shadow across the area (photo Patrick L. Colin).

become light-limited on a slope that is shaded for much of the

day (Figure 2.11).

Mesophotic corals exhibit several adaptations relative to

dependence on low light at depth, one of which is the switch

from autotrophic (i.e., energy from light) to heterotrophic

(i.e., energy from consumed foods) nutrition. This has been

demonstrated using stable isotope techniques in scleractinian

corals,

Montastraea cavernosa

(Lesser et al. 2010) and in

a facultative zooxanthellate gorgonian from a temperate

ecosystem (Gori et al. 2012). Specifically, planktonic

resources, which are often higher on mesophotic reefs (e.g.

Lesser and Slattery 2013) due to upwelled nutrients (Leichter

and Genovese 2006, Leichter et al. 2007), are captured by the

coral’s tentacles, thereby offsetting the lmss of energy from

phototrophic sources.

Figure 2.10.

The absorption of light is influenced by the micromorphology of coral and algal skeletons.

Source: Enríquez et al. 2005, Kahng et al. 2012a, Kahng 2014

Porites

structure

Leptoseris

structure

Flat skeleton

Leaf

E ect of morphology on light harvesting

Water column

Tissue

Coral skeleton

Sunlight