Conclusions
Reef building in the Mariana Islands is confined to the
inactive southern Arc from Guam to Farallon de
Medinilla.
The dominant coral reef type in the Marianas is fringing
reefs, with barrier reefs only at Guam (Cocos Lagoon)
and Saipan (Tanapag Lagoon).
The northern Marianas are volcanically active and
corals occur there, but tectonic instability and volcanic
activity have precluded reef building.
Reef building in the southern Marianas likely dates
back to the Miocene, but no reef edifice has yet been
found (corals and reefal fragments only).
Late Holocene reef building in the southern Marianas is
constrained by the presence of an early Holocene reef
episode (Merizo Limestone on Guam, Milencattan
Limestone on Rota, and younger part of Tanapag Limestone on Saipan) that clearly shows a mid-Holocene
sea-level overshoot.
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