malaysia_ioc-westpac 2016 new

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Current status of implementation for OA studies in Malaysia

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Page 1: Malaysia_IOC-Westpac 2016 new

CurrentstatusofimplementationforOAstudiesinMalaysia

Page 2: Malaysia_IOC-Westpac 2016 new

LocationoftheproposedstudysiteN

400km

Pulau Gaya

STUDYSITE

Sumatra

PulauPayar

TarutaoNationalPark

SOUTHCHINASEA

PulauBidong

Page 3: Malaysia_IOC-Westpac 2016 new

P.Payar

P.Lembu

P.Kaca

N

STRAITOFMALACCA

1km

MarineParkCentre

PulauPayarMarinePark

Page 4: Malaysia_IOC-Westpac 2016 new

Pulau Bidong (UMTMarineResearchStation)

UMTMarineResearchStation

N

SOUTHCHINASEA

1km

Page 5: Malaysia_IOC-Westpac 2016 new

InvestigatingthediurnalvariationoftheseawaterpHandalkalinityinshallowwatercoralreefofPulau Payar (StraitofMalacca),Pulau Bidong andPulau Gaya(SouthChinaSea)astheproposedsitesoftheocean

acidificationstudy.

Page 6: Malaysia_IOC-Westpac 2016 new

DiurnalvariabilityofpHandtotalalkalinity

3dayperiodofobservationatashallowwater coralreefarea

In-situmeasurement&watersamplecollection

Every3hours,watersamplewerecollectedandmeasuredfortheTotalAlkalinity(AT)

HydrolabDS5Xrecordedreadingevery15minute(pH,Temperature,Salinity,DissolvedOxygen,DO)

AragonitesaturationweredeterminedusingtheCO2SYSprogram(LewisandWallace,1998)throughinsituAT,pH,

salinity,temperaturedata.

Page 7: Malaysia_IOC-Westpac 2016 new

Methodsthatwereusedtodeterminetheseawatercarbonateparameter

Parameters Unit MeasurementMethods

Temperature °C HydrolabDS5X

Salinity ppt HydrolabDS5X

pH HydrolabDS5X

DissolvedOxygen(DO) mg/L HydrolabDS5X

TotalAlkalinity µmol/kg PotentiometricTitration(Dicksonetal.2007)

AragoniteSaturation ΩAragonite CO2SYSprogram(LewisandWallace,1998)

Page 8: Malaysia_IOC-Westpac 2016 new

DiurnalvariationinseawaterpHatthestudyarea

day day daynight night night

• pH trend fluctuates daily following the diurnal pattern which is regulated by the biological activity such as photosynthesis and respiration

Payar(SOM)

Bidong(SCS)

Gaya(SCS)

Page 9: Malaysia_IOC-Westpac 2016 new

SeawaterpHatPulauPayar,PulauBidongandPulauGaya

• Decreasing surface seawater pH trend from the Strait of Malacca to the South China Sea

morebasic

lessbasic

Page 10: Malaysia_IOC-Westpac 2016 new

Diurnalvariationoftotalalkalinity

day day daynight night night

Payar(SOM)

Bidong(SCS)

Gaya(SCS)

• Total alkalinity (AT) did not show any diurnal trend through out this study.• However, the largest difference of AT was recorded at Payar with the value of 28.92 μmol/kg.• Changes in AT are attributed to calcification or carbonate dissolution (Murillo et al., 2014)

Page 11: Malaysia_IOC-Westpac 2016 new

Relationshipbetweentotalalkalinityandsalinity

• Precipitation and evaporation mainly controls the AT variability of surface ocean (Brewer et al., 1986; Millero et al., 1998a)

• Concentrations of the key chemical species (i.e., HCO3

-

CO32-) that contribute to AT

proportionally increase with increasing salinity (Lee et al., 2006)

Page 12: Malaysia_IOC-Westpac 2016 new

CO2 ParameterVariation

• pH ranged 7.21 to 7.81°C• Lower pH observed at the southern

region

pH

• ρCO2 ranged 710 to 3151 µatm

• Higher ρCO2 observed at the southern region

ρCO2 (µatm)

Page 13: Malaysia_IOC-Westpac 2016 new

• Aragonite saturation ranged 0.57 to 2.26• Low saturation state observed at the

southern region• At extremely marginal state

Aragonite Saturation (ΩAra)

CO2 ParameterVariation

Hoegh-Guldberg et al. 2007: Ωarag = 3.3

Shamberger et al. 2011

Saturation States in the Pacific

(Shambergeretal.2011)

(ReefsatRiskRevisited 2011)

Saturation state in our region

Page 14: Malaysia_IOC-Westpac 2016 new

Carbonateenvironmentcomparison• Pulau Bidong and Pulau Gaya

– Higher AT were recorded at these sites, 2161.78 μmol kg-1 and2160.45 μmol kg-1 respectively.

– The pH at both sites are lower than Payar as denoted by the higherH+ concentration in the seawater.

– Aragonite saturation in the seawater at both sites were recorded atadequate (3.41) and marginal (2.99) level respectively.

• Pulau Payar– Lower AT (2140.77 μmol kg-1) means the capacity of the seawater

buffer system to neutralize acidic pollution is reduced.– At present, the seawater carbonate system is maintained because of

the pH value (pH 8.14).– Only a small amount of acidic pollution is needed to disrupt the

carbonate system equilibrium.– Optimal aragonite saturation state in Payar contributes to the high

coral calcification rate in the area.

Page 15: Malaysia_IOC-Westpac 2016 new

CurrentstatusofimplementationforOAstudiesinMalaysia

• AllrequiredCAUs,BMUsandARMshavebeenmanufacturedbutasyetnotdeployed

• diurnalvariationsurveyofselectedstationhasbeencompletedfortemperature,salinity,pHDO,aragonitesaturationandtotalalkalinity

• Coralcoveranddiversitystudiesareplannedfor2016-2017).Bioticsurvey(georeferenced,cover,diversity)iscurrentlybeinganalysed.

Page 16: Malaysia_IOC-Westpac 2016 new

• Localorganizingcommittee• IOC/WESTPAC• Mr.WenxiZhu• PhuketMarineBiologicalStation