may record several such events. Accordingly, in appropriate settings, the periodicity of relatively minor volcanic
events may be established in the fossil record with much
greater precision than previously permitted.”
How to identify if a reef is sediment-stressed
Globally, coral reefs are threatened by a plethora of
anthropogenic and natural factors, and many reefs face
multiple stressors (Hughes and Connell, 1999).
Disentangling sedimentation from the other stressors with
which it usually co-occurs is quite difficult (Fabricius,
2005). The following factors typically occur on reefs subject to sedimentation, with or without other stressors:
1. High siliciclastic content in reef sediment
2. High insoluble residue content in coral skeletons, particularly open-lattice species like massive Porites
3. High Ba/Ca ratio in coral skeletons
4. Low recruitment rates of corals, often resulting in size
distributions skewed to large colonies
5. Low species diversity of corals, relative to reference
sites in same region
6. Low percentage live coral cover, combined with high
cover of dead coral (high mortality index)
7. Predominance of stress-tolerant coral species and
growth forms, especially multilobate massive colonies
8. High-extension, low-density skeletal growth
Summary
Sediment input is one of the great killers of coral reefs.
The effect is accentuated, because in most situations the
sediment is accompanied by dissolved nutrients and
organic matter. In many cases, however, the source and
the nature of the stress may be identified using a variety
of geochemical techniques.
Acknowledgments
The senior author performed much of the work for this
article whilst in residence as a Temminck Fellow at the
Natural History Museum in Leiden, Netherlands.
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