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MESOPHOTIC CORAL ECOSYSTEMS – A LIFEBOAT FOR CORAL REEFS?

81

6.7.3.

The Green Alga

Avrainvillea

sp.

Avrainvillea

sp., an invasive green alga (Figure 6.18) known

for its propensity to displace native seagrass populations in

the intertidal zone (Peyton 2009), was first reported in Hawai‘i

in 1981 in 13 m of water off Kahe Point, O‘ahu (Brostoff 1989),

and is now found offshore of O‘ahu at depths to 90 m (Peyton

2009, Spalding 2012). Originally identified as

Avrainvillea

amadelpha

, recent research suggests that this identification is

incorrect and work is now underway to confirm the invasive

alga’s identity (A. Sherwood pers. com.).

The

Avrainvillea

sp. spread from its first collection site at Kahe

Point toMaunalua Bay (50 kmdistance) within about six years

(Brostoff 1989). Presently, the distribution of this species in

Hawai‘i extends along most of O‘ahu’s southern and western

shores, and has been documented in a one-time collection

from Kaua‘i (Smith et al. 2002). The mechanism(s) of its

rapid propagation is not known. The species’ high abundance

at mesophotic depths introduces the possibility that it may

have originated in mesophotic waters and then moved into

shallower waters (Spalding 2012).

Some species of

Avrainvillea

form dense mats on either hard

or soft substrata. These mats sequester fine sediments under

their holdfast structures (Littler et al. 2005), creating anoxic

mounds of soft sediment in otherwise hard-substratum-

dominated environments (H. Spalding pers. obs.). Within

its natural range, members of the genus

Avrainvillea

have been found at mesophotic depths in Mauritius (

A.

amadelpha

) at 90 m (Gepp and Gepp 1911) and on a

Bahamian seamount (

A. levis

) at 125 m (Littler and Littler

1992). Despite its high abundance around west and south

O‘ahu,

Avrainvillea

sp. has not yet been found in the nearby

‘Au‘au Channel (located between the islands of Lāna‘i and

Maui), which contains extensive MCEs, and its competitive

impact on dominant native mesophotic macroalgae, such as

Halimeda kanaloana

meadows in this region is unknown.

The high abundance and ability of

Avrainvillea

sp. to grow

on a diversity of substrata types increases the likelihood of

its transport between the islands by potential transfer on

construction materials for underwater development, such as

pipelines, or by attachment to boat anchors. Removal efforts

for mesophotic populations of

Avrainvillea

sp. would be

costly and difficult, highlighting the need to limit the spread

of this highly adaptable and invasive algal species.

Lionfish are now common throughout the Western Atlantic

Ocean, theGulf of Mexico andCaribbean.The first sightings in the

Gulf of Mexico occurred in 2010, with lionfish populations having

since increased dramatically on many shallow and mesophotic

reefs. During submersible dives in 2010, only a few lionfish were

documented along the West Florida Shelf MCEs in the Gulf of

Mexico (Reed and Rogers 2011) and none were reported in the

same region in 2003 (by a United States Geological Survey study).

However, by 2013, a total of 703 lionfish were observed during

remotely operated vehicle surveys at Pulley Ridge, a MCE (60–

80 m depth) on the West Florida Shelf (Reed et al. 2014; Figure

6.17). Of the 33 1–km

2

blocks surveyed at Pulley Ridge, 72 per

cent contained lionfish, most of which were associated with

active red grouper,

Epinephelus morio,

burrows. Burrows (5–15 m

in diameter) are excavated by red grouper and provide habitat

and act as oases for many small reef fish and lionfish. From

multibeam sonar maps of Pulley Ridge, over 136,000 red grouper

burrows are visible in the region, providing the potential for tens

of thousands of lionfish.

Lionfish on the Pulley Ridge mesophotic reef in the Gulf of Mexico

Figure 6.17.

The invasive lionfish has been found in increasing

numbers at red grouper burrows at Pulley Ridge at 70 m (photo

John Reed, NOAA Coral EcosystemConnectivity Expedition 2014).

Figure6.18.

Avrainviella

sp., an invasive green alga at 50m, is found

offshore of O‘ahu’s southern and western shores from shallow to

mesophotic depths. The diver is measuring the sediment depth

under the algal mat. This species has the potential to transform a

diverse, coral-dominated area into dense mats of macroalgae over

anoxic mounds of sediment (photo Heather Spalding).