a reflection of the underlying antecedent substrate –
a position that would surely have Darwin turning in his
grave. Although examples do exist of this substrate control, scaling-up of the concept to entire reef systems denies
abundant evidence that reefs have built impressively thick,
well-structured edifices during the last 14 ka, which have
maintained their breakwater position as post-glacial sea
level rose 120 m or more from its glacial low-stand. An
understanding of the interactions and feedbacks that control reef organization during this development is key to
assessing resilience and resistance of modern reef systems
in the face of human-induced global environmental
change.
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