Balanus crenatus

Researched ByNicola WhiteData Supplied ByMarLIN
Refereed byProf. Alan J. Southward
Taxonomy
Scientific nameBalanus crenatusCommon nameAn acorn barnacle
MCS CodeR77Recent SynonymsNone
PhylumCrustaceaSubphylum
SuperclassClassMaxillopoda
SubclassCirripediaOrderThoracica
SuborderBalanomorphaFamilyBalanidae
GenusBalanusSpeciescrenatus
Subspecies  
Additional InformationNo text entered
Taxonomy References Rainbow, 1984, Bassindale, 1964
General Biology
Growth formConicalFeeding methodPassive suspension feeder, Active suspension feeder
Mobility/MovementPermanent attachmentEnvironmental positionEpifaunal, Epilithic
Typical food typesZooplankton and other organic particles of a suitable size, such as detritus and phytoplankton.HabitAttached
BioturbatorNot relevantFlexibilityNone (< 10 degrees)
FragilityRobustSizeSmall(1-2cm)
HeightInsufficient informationGrowth Rate4.4 mm/month
Adult dispersal potentialNoneDependencyIndependent
SociabilityGregarious
Toxic/Poisonous?No
Additional InformationBalanus crenatus has a calcareous base, while Semibalanus balanoides has a membranous base.
Feeding
Balanus crenatus feeds by extending thoracic appendages called cirri out from the shell to filter zooplankton from the water. In the absence of any current, the barnacle rhythmically beats the cirri. When a current is present Balanus crenatus holds the cirri fully extended in the current flow. Barnacles feed most during spring and autumn when plankton levels are highest. Little if any feeding takes place during winter, when barnacles rely on stored food reserves. Feeding rate is important in determining the rate of growth.
Moulting
Barnacles need to moult in order to grow. Frequency of moulting is determined by feeding rate and temperature. Moulting does not take place during winter when phytoplankton levels and temperatures are low.
Size:
Balanus crenatus is hermaphroditic and grows up to 25mm in diameter.
Biology References Rainbow, 1984, Barnes et al., 1963, Bassindale, 1964
Distribution and Habitat
Distribution in Britain & IrelandAll coasts of Britain & Ireland, and offshore in the North Sea and Celtic Sea.
Global distributionNortheast Atlantic from the Arctic to the west coast of France as far south as Bordeaux; east and west coasts of North America and Japan.
Biogeographic rangeNot researchedDepth rangeInsufficient information
MigratoryNon-migratory / Resident
Distribution Additional InformationBalanus crenatus is a widespread species that occurs at quite high latitudes in the Arctic. It colonizes a wide range of substrata, attaching to any hard substrata, molluscs and their dead shells (Southward, pers. comm.), often as an initial colonizing species. Densely packed colonies occur particularly in areas exposed to strong tidal streams where few other epifauna survive. It can also be found attached to carapaces of the Norway lobster or Dublin Bay prawn (Nephrops norvegicus) and other crustaceans.
Balanus crenatus may have been misidentified as Solidobalanus fallax in shallow waters lying to the south of the UK. The deep water record of Gruvel (noted in Southward, 1998) is an error (Southward, pers. comm.). Balanus crenatus and Solidobalanus fallaxcolonize different substrates and also occur in different temperatures. Solidobalanus fallax occurs in warmer water on shells, false corals, seaweeds and other soft substrata, including plastic bags and synthetic netting (Southward, pers. comm.).
Substratum preferencesBedrock, Artificial (e.g. metal/wood/concrete), Cobbles, Gravel / shingle, Large to very large boulders, Pebbles, Small bouldersPhysiographic preferencesOpen coast, Offshore seabed, Strait / sound, Sealoch, Ria / Voe, Estuary, Enclosed coast / Embayment
Biological zoneLower Eulittoral, Sublittoral Fringe, Upper Infralittoral, Lower InfralittoralWave exposureExtremely Exposed, Very Exposed, Exposed, Moderately Exposed, Sheltered, Very Sheltered, Extremely Sheltered
Tidal stream strength/Water flowVery Strong (>6 kn), Strong (3-6 kn), Moderately Strong (1-3 kn), Weak (<1 kn), Very Weak (negligible)SalinityFull (30-40 psu), Reduced (18-30 psu), Variable (18-40 psu), Low (<18 psu)
Habitat Additional Information
Distribution References Rainbow, 1984, Barnes, 1953, Barnes et al., 1963, JNCC, 1999, Bassindale, 1964, Southward, 1998
Reproduction/Life History
Reproductive typePermanent hermaphrodite Developmental mechanismPlanktotrophic, Lecithotrophic
Reproductive SeasonFebruary to SeptemberReproductive LocationAs adult
Reproductive frequencyAnnual episodic Regeneration potentialNo
Life span1-2 yearsAge at reproductive maturity<1 year
Generation time<1 yearFecundityInsufficient information
Egg/propagule sizeInsufficient informationFertilization type
Larvae/Juveniles
Larval/Juvenile dispersal potential>10kmLarval settlement periodInsufficient information
Duration of larval stage11-30 days  
Additional Information
  • Balanus crenatus is an obligate cross-fertilizing hermaphrodite. Nauplii larvae are released from the barnacle between February and September, with peaks in April and late summer when phytoplankton levels are highest. However, release is not synchronised with the spring algal bloom, unlike Semibalanus balanoides.
  • Nauplii larvae are planktotrophic and develop in the surface waters. They pass through six nauplii stages before eventually developing into a cyprid larva. Cyprid larvae are specialised for settlement. They drift and swim in the plankton before selecting a suitable substratum for settlement and metamorphosis. Peak settlement occurs in April and declines until October. Metamorphosis usually takes place within 24 hours of settlement.
  • Barnacles grow rapidly except in winter. April-settled individuals may release larvae the same July and reach full size before their first winter. Individuals that settled later reach maximum size by the end of spring the following year (Rainbow, 1984).
  • Balanus crenatus has a life span of 18 months (Barnes & Powell, 1953). Growth rate varies greatly with the degree of current flow and the presence of silt. Balanus crenatus populations attached to Nephrops norvegicus grew only 2mm in 4 months, whereas populations on rafts grew at 0.2mm per day. This reduction in growth in epizoic populations is attributed to the higher presence of silt and reduction in water currents (Barnes & Bagenal, 1951).
Reproduction References Rainbow, 1984, Barnes & Powell, 1953, Barnes & Bagenal, 1951