Spatial Variation in Biofouling of a Unionid Mussel (Lampsilis siliquoidea) Across the Western Basin of Lake Erie Data
Invasion of North American waters by Dreissena polymorpha and
D. rostriformis bugensis has resulted in declines in native North
American Unionoida mussels. Dreissenid mussels biofoul unionid
mussels in large numbers and interfere with unionid movement,
acquisition of food and ability to open and close their shells.
Initial expectations for the Great Lakes were that unionids would be
extirpated where they co-occur with dreissenids, but recently adult
and juvenile unionids have been found alive in several apparent
refugia. These unionid populations may persist due to reduced
dreissenid biofouling in these areas, and/or due to processes that
remove biofoulers. For example, locations inaccessible to veligers
may reduce biofouling and habitats with soft substrates may allow
unionids to burrow and thus remove dreissenids. Here, biofouling was
measured by deploying caged unionid mussels (Lampsilis siliquoidea) at
36 sites across the western basin of Lake Erie to assess spatial
variation in biofouling and to identify other areas that might promote
the persistence or recovery of native unionid mussels. Biofouling
ranged from 0.03 – 26.33 g per mussel, reached a maximum in the
immediate vicinity of the Maumee rivermouth, and appeared to primarily
consist of dreissenid mussels. A known mussel refugium in the
vicinity of a power plant near the Maumee rivermouth actually
exhibited very high biofouling rates, suggesting low dreissenid
colonization is unlikely to be the primary cause of unionid survival
in this refugium. The southern nearshore area of Lake Erie, near
another refugium, also had very low biofouling. A large stretch of the
western basin appeared to have low biofouling rates and muddy
substrates, raising the possibility that these open water areas could
support remnant and returning populations of unionid mussels.
Complete Metadata
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| description | Invasion of North American waters by Dreissena polymorpha and D. rostriformis bugensis has resulted in declines in native North American Unionoida mussels. Dreissenid mussels biofoul unionid mussels in large numbers and interfere with unionid movement, acquisition of food and ability to open and close their shells. Initial expectations for the Great Lakes were that unionids would be extirpated where they co-occur with dreissenids, but recently adult and juvenile unionids have been found alive in several apparent refugia. These unionid populations may persist due to reduced dreissenid biofouling in these areas, and/or due to processes that remove biofoulers. For example, locations inaccessible to veligers may reduce biofouling and habitats with soft substrates may allow unionids to burrow and thus remove dreissenids. Here, biofouling was measured by deploying caged unionid mussels (Lampsilis siliquoidea) at 36 sites across the western basin of Lake Erie to assess spatial variation in biofouling and to identify other areas that might promote the persistence or recovery of native unionid mussels. Biofouling ranged from 0.03 – 26.33 g per mussel, reached a maximum in the immediate vicinity of the Maumee rivermouth, and appeared to primarily consist of dreissenid mussels. A known mussel refugium in the vicinity of a power plant near the Maumee rivermouth actually exhibited very high biofouling rates, suggesting low dreissenid colonization is unlikely to be the primary cause of unionid survival in this refugium. The southern nearshore area of Lake Erie, near another refugium, also had very low biofouling. A large stretch of the western basin appeared to have low biofouling rates and muddy substrates, raising the possibility that these open water areas could support remnant and returning populations of unionid mussels. |
| distribution |
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[
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| modified | 2021-05-06T00:00:00Z |
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[
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|
| title | Spatial Variation in Biofouling of a Unionid Mussel (Lampsilis siliquoidea) Across the Western Basin of Lake Erie Data |