Seawater carbon chemistry and regenerative capacity of in adult sea urchins spines and tube feet

Increasing atmospheric carbon dioxide (CO2) has resulted in a change in seawater chemistry and lowering of pH, referred to as ocean acidification. Understanding how different organisms and processes respond to ocean acidification is vital to predict how marine ecosystems will be altered under future...

Full description

Bibliographic Details
Main Authors: Emerson, Chloe E, Reinardy, Helena C, Bates, Nicolas R, Bodnar, Andrea G
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
Alkalinity
total
standard error
Animalia
Aragonite saturation state
Barium/Calcium ratio
Behaviour
Benthic animals
Benthos
Bicarbonate ion
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Category
Coast and continental shelf
Conductivity
Containers and aquaria (20-1000 L or < 1 m**2)
Echinodermata
EXP
Experiment
Experiment duration
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gene expression
fold change
relative
Ocean acidification
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.878254
https://doi.org/10.1594/PANGAEA.878254

Similar Items