BIO 475 Lecture 18: Mesophotic Reefs

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13 Jun 2018
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Mesophotic Reefs
Top Mesophotic zone ~ 30m
Bottom mesophotic ~150-200m
Set by light availability
Shallow water coral reefs on trajectory to decline and degrade
Deeper you go, less effect on corals (water temp and other anthropogenic _
Mesophotic reefs could serve as refuge
Deeper depths, reefs have better chance of survival
Submersible Surveys
Manned submersibles 2-3 people
Take notes and video on what they see
Arm to take samples
ROV’s
Specimen collection
HD cameras
Monitor physical environment with glider
Take measurements of pH, salinity, conductivity, echo sounds, plankton
abundance
Can’t take samples
In Situ Surveys
Technical diving
Nitrox
Really deep depths require Helium; trimix
Have to switch gasses as you ascend to aid in decompression
Rebreather
Stay deeper and longer
Recycle air you're breathing
Could breathe off the tanks for 8 hours
Mesophotic vs shallow
Shallow - surface to 30m
Dominated by symbiotic scleractinian coral and octo corals, algae and
sponges
Lighter
Stratified water with high residence times
Extreme highs, extreme lows
High turbulence and waves breaking (suspended sediment )
Mesophotic coral ecosystems (MCEs) - 30 to 40m
Corals become more plate like, less abundant, black corals, more algae
and sponges
Darker
Variable temperatures regimes, oscillations of deep water waves, and
upwelling
Dissipated turbulence with depth
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Document Summary

Shallow water coral reefs on trajectory to decline and degrade. Deeper you go, less effect on corals (water temp and other anthropogenic _ Deeper depths, reefs have better chance of survival. Take notes and video on what they see. Take measurements of ph, salinity, conductivity, echo sounds, plankton abundance. Have to switch gasses as you ascend to aid in decompression. Could breathe off the tanks for 8 hours. Dominated by symbiotic scleractinian coral and octo corals, algae and sponges. High turbulence and waves breaking (suspended sediment ) Mesophotic coral ecosystems (mces) - 30 to 40m. Corals become more plate like, less abundant, black corals, more algae and sponges. Variable temperatures regimes, oscillations of deep water waves, and upwelling. As sea levels rose, reefs deposited along higher slope, sea level rises more and you get inshore reefs, and continues to rise; now the mce"s becoming deep. Couldn"t keep up with sea level rising. Reef environment and light reaching the mesophotic zone.

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