Seawater carbonate chemistry and maximum quantum yield and relative electron transfer rate of microalgal communities in Antarctic pack ice

Increased anthropogenic CO2 emissions are causing changes to oceanic pH and CO2 concentrations that will impact many marine organisms, including microalgae. Phytoplankton taxa have shown mixed responses to these changes with some doing well while others have been adversely affected. Here, the photos...

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Bibliographic Details
Main Authors: Coad, Thomas, McMinn, Andrew, Nomura, Daiki, Martin, Andrew
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
Alkalinity
total
Antarctic
Aragonite saturation state
Bicarbonate ion
Bottles or small containers/Aquaria (<20 L)
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Chlorophyll a
Comment
Entire community
Event label
EXP
Experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Incubation duration
Laboratory experiment
Light saturation
Maximal electron transport rate
relative
Maximum quantum yield of photosystem II
OA-ICC
Ocean Acidification International Coordination Centre
Open ocean
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Pelagos
pH
Photosynthetic quantum efficiency
Polar
Primary production/Photosynthesis
Salinity
SIPEX-2_station__4
SIPEX-2_station__7
SIPEX-2_station__8
Station label
Temperature
water
Treatment
Type
Antarc*
ice algae
Ocean acidification
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.933802
https://doi.org/10.1594/PANGAEA.933802

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