MESOPHOTIC CORAL ECOSYSTEMS – A LIFEBOAT FOR CORAL REEFS?
10
bleaching event, than adjacent shallow reefs (Bongaerts et al.
2010a, Bridge et al. 2014). MCEs may have the potential to
act as refugia over longer timescales in some circumstances,
particularly to provide lineage continuation for key coral reef
taxa (Muir et al. 2015).
Currently, few long-term datasets exist to enable quantitative
evaluation of the deep reef refugia hypothesis, particularly
over longer temporal scales (years to decades), primarily due
to the logistical difficulties involved inmonitoringmesophotic
habitats. There is evidence that mesophotic reef populations
can mitigate against local extinction following disturbance
(e.g. Sinniger et al. 2013, Smith et al. 2014). However, it
is also clear that MCEs are not immune from natural and
human threats, such as coral bleaching and tropical storms
(see Chapter 6), and should not be considered as a panacea
to addressing the threats faced by coral reef ecosystems. For
example, bleaching of MCEs is known to occur where internal
waves or vertical mixing brings over-heated surface waters or
cooler deep waters into contact with mesophotic corals (Bak
et al. 2005, Smith et al. 2015).
In addition to serving as a refuge, a second premise of the
deep reef refugia hypothesis is whether MCEs can provide a
source of larvae to repopulate adjacent shallow reefs following
a disturbance on ecologically significant timescales. The
viability of MCEs to serve as a source to reseed or replenish
shallow reef species is dependent on several factors, including
Figure 1.1.
Impacts of human and natural disturbances tend to decrease with depth and distance from the coast, making shallow reefs
generally more vulnerable than MCEs.
whether the same species are present at both depths, the extent
of species adaptation at particular depths, and whether there
is oceanographic connectivity between the reefs. Studies
addressing this question for coral species have, to date,
generally looked at genetic connectivity between mesophotic
and shallow populations, and have revealed complex patterns.
In general, deeper mesophotic coral populations (> 60–70 m
in depth) appear to be isolated from shallower populations
(Bongaerts et al. 2015b). In contrast, coral connectivity
between populations shallower than 60–70 m appears to
be both species and location-specific and dependent on
oceanographic connectivity (van Oppen et al. 2011, Serrano
et al. 2014). For fish species, connectivity has been evaluated
using genetics and ecology (presence of the same species at
both depths). In the case of the common coral reef damselfish,
Chromis verater
, no genetic differences were found among
shallow and mesophotic populations (Tenggardjaja et al.
2014), meaning they constitute a single population and should
be managed as such. Meanwhile, ecological connectivity has
been shown for fish species between shallow reefs and MCEs
off La Parguera in southwest Puerto Rico. These MCEs serve as
a refuge, particularly for exploited large groupers and snappers,
and 76 per cent of species present at mesophotic depths
were common inhabitants of shallow reefs, indicating that
connectivity exists between shallow reefs and MCEs (Bejarano
et al. 2014). Irrespective of their potential to repopulate
shallow-water reefs, MCEs support unique biodiversity and
warrant appropriate attention from managers.
Interconnection between land and shallow-water and mesophotic reefs
- the impacts of human and natural disturbances on coral reefs tend to diminish with depth and distance from shore
Sedimentation (e.g. from rivers,
coastal development) and
shing pressure diminish with
distance from shore
Storms diminish
with depth
0m
60m
Sediment plume
Source: Adapted from Bridge et al. 2013