Carbonate chemistry, temperature and salinity of Lady Elliot Island Reef 2009-2010

Ocean acidification leads to changes in marine carbonate chemistry that are predicted to cause a decline in future coral reef calcification. Several laboratory and mesocosm experiments have described calcification responses of species and communities to increasing CO2. The few in situ studies on nat...

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Bibliographic Details
Main Authors: Shaw, Emily, McNeil, Ben I, Tilbrook, Bronte
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
Alkalinity
total
Carbon
inorganic
dissolved
DATE/TIME
Date/time start
DEPTH
water
Event label
Great Barrier Reef
Australia
LEI_offshore
LEI_reef-flat
Salinity
Temperature
Water sample
WS
Elliot
Ocean acidification
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.823685
https://doi.org/10.1594/PANGAEA.823685

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