hat
Nan balans lokal yo, lanmè-nivo monte se chans ogmante pwosesis sedimantè ki potansyèlman entèfere ak fotosentèz, manje, rekritman, ak lòt pwosesis kle refe fizyolojik. ref Pa egzanp, li ka lakòz sedimantasyon ogmante akòz ewozyon plaj ki ta ka toufe resif yo oswa redwi limyè solèy la ki nesesè pou fotosentèz. Menm ogmantasyon ti nivo lanmè a (pa egzanp, 0.2) ka ogmante turbidite sou resif fringing nan de mekanism: 1) ogmante re-sispansyon nan sediman amann sou plat Reef (pòsyon an enteryè nan resif franje pi pre sous sediman) ak 2) ogmante ewozyon kotyè ak transpò amann sediman nan resif adjasan. Anlèvman nan estrikti Reef te mennen nan yon retrè rapid nan resif pandan rapid la ak gwo (XN) nivo lanmè-monte nan enteryè a dènye. ref
eng
At local scales, sea-level rise is likely to increase sedimentary processes that potentially interfere with photosynthesis, feeding, recruitment, and other key physiological reef processes. ref For example, it can cause increased sedimentation due to shoreline erosion which could smother reefs or reduce sunlight needed for photosynthesis. Even small increases in sea level (e.g., 0.2 m) can increase turbidity on fringing reefs through two mechanisms: 1) increased re-suspension of fine sediment on reef flats (the inner portion of fringing reefs closer to sediment sources) and 2) increased coastal erosion and transport of fine sediment to adjacent reefs. Smothering of reef structures led to a rapid retreat of reefs during the rapid and large (6 m) sea-level rise of the last interglacial. ref