Seawater carbonate chemistry and Antarctic macroalgal biochemical composition and amphipod grazer feeding preferences

Increased anthropogenic atmospheric CO2 concentrations have resulted in ocean warming and alterations in ocean carbonate chemistry, decreasing seawater pH (ocean acidification). The combination of ocean warming and acidification (OWA) may alter trophic interactions in marine benthic communities alon...

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Bibliographic Details
Main Authors: Schram, Julie B, Schoenrock, Kathryn M, McClintock, James B, Amsler, Charles D, Angus, Robert A
Format: Dataset
Language:English
Published: PANGAEA 2017
Subjects:
Alkalinity
total
standard deviation
Animalia
Antarctic
Aragonite saturation state
Arthropoda
Behaviour
Benthic animals
Benthos
Bicarbonate ion
Biomass/Abundance/Elemental composition
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Chromista
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Date
Desmarestia anceps
Desmarestia menziesii
EXP
Experiment
Experiment duration
Feeding rate
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gondogeneia antarctica
Identification
Laboratory experiment
Lipids
Macroalgae
Mass
Mass change
OA-ICC
Ocean Acidification International Coordination Centre
Antarctic Peninsula
Antarc*
Antarctica
Ocean acidification
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.892654
https://doi.org/10.1594/PANGAEA.892654

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