Skip to main content

Table 1 Seawater chemistry parameters during the experiment (mean ± SD)

From: Combined effects of ocean acidification and hypoxia on the early development of the thick shell mussel Mytilus coruscus

DO (mg/L)

pHNBS

Salinity

T (°C)

TA (μmol/kg)

DIC (μmol/kg)

pco2 (μatm)

Ωcal

Ωara

6.1 ± 0.1

7.33 ± 0.03

25.1 ± 0.1

20.0 ± 0.1

2316 ± 11

2343 ± 22

2715 ± 23

1.04 ± 0.08

1.19 ± 0.05

2.0 ± 0.2

7.30 ± 0.01

25.2 ± 0.1

20.1 ± 0.2

2345 ± 28

2379 ± 32

2939 ± 18

1.01 ± 0.03

1.22 ± 0.01

6.0 ± 0.1

7.69 ± 0.02

25.1 ± 0.3

20.0 ± 0.2

2376 ± 11

2224 ± 19

1015 ± 10

1.77 ± 0.04

1.24 ± 0.06

2.0 ± 0.2

7.70 ± 0.01

25.1 ± 0.2

20.0 ± 0.1

2295 ± 39

2114 ± 15

995 ± 11

1.84 ± 0.17

1.19 ± 0.03

6.1 ± 0.1

8.09 ± 0.02

25.0 ± 0.1

19.9 ± 0.2

2241 ± 41

1994 ± 19

351 ± 21

4.39 ± 0.07

2.76 ± 0.09

2.1 ± 0.1

8.10 ± 0.02

25.0 ± 0.1

20.0 ± 0.1

2208 ± 20

2059 ± 31

373 ± 12

4.40 ± 0.10

2.91 ± 0.07

  1. pH was monitored by the pH/CO2 system continuously during the experiment. Salinity, temperature and total alkalinity (TA) were determined at each sampling time (n = 5). Dissolved inorganic carbon (DIC), partial pressure of CO2 (pCO2), saturation degrees for calcite ( Ωcal) and aragonite (Ωara) were calculated based on the above parameters