Ocean acidification (pH 7.7) impaired growth and development of an intertidal barnacle (Semibalanus balanoides), but warmer temperature (+4 °C) did not. The mineral composition of the shells did not change with either ocean acidification or warmer temperature. The combination of reduced growth and maintained mineral content suggests that the barnacles shifted their energy from growth toward maintaining their shell, as ocean acidification makes the shell prone to dissolving. (Laboratory study)
Author(s): Findlay, H.S.
Date: 2010
Link: https://www.sciencedirect.com/science/article/abs/pii/S0272771409005629
Overview:
Educational Materials
Scientific Literature
Additional Topics:
Aquaculture
Biological effects of OCA
Calcification
Ecosystem
Ecosystem services
Food quality/availability
Food web
Freshwater inputs
Growth
Intergenerational effects
Mortality
Multiple stressors
Reproduction
Seasonality
Geographic Areas:
Caribbean
East Coast
Global
Gulf of Maine
Gulf of Mexico
Northeast U.S.
Scotian Shelf
West Coast
Life Stages:
Adults
Eggs
Juveniles
Larvae
Marine Life:
Crustaceans
Fish
Mollusks
Other
Other invertebrates
Phytoplankton
Seaweed and seagrasses
Zooplankton
Parameters:
CaCO3 saturation state
Carbonate chemistry
CO2 / pCO2
Nutrients
pH
Salinity
Temperature
Species Group:
Barnacles
Clams
Cod
Copepods
Coralline algae
Crabs
Diatoms
Lobster
Mussels
Oysters
Pteropods
Scallops
Sea stars
Sea urchins
Shellfish
Shrimp
Squid
Summer flounder
Tube worms