photosynthesis of seagrass

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  • 7/29/2019 Photosynthesis of Seagrass

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    Indian Journal of Marine SciencesVol. 30 (4), December 2001, pp. 253-256

    Short Communication

    Photosynthesis of seagrass Cymodocea serrulata (Magnoliophyta/

    Potamogetonales/Cymodoceaceae)in field and laboratory

    M K Abu Hena *, K Misri, B Japar Sidik, O Hishamuddin & H HidirDepartment of Biology, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor D E, Malaysia

    Received 27 February 2001, revised 20 August 2001

    In situ photosynthetic study for seagrass Cymodocea serrulata at two depths (0.5 m, 2.0 m) at Port Dickson, Negeri

    Sembilan was conducted. The photosynthetic rate at 0.5 m was comparatively higher (0.4760.080 mg O2/hr/g fr wt or

    0.5710.182 g O2/hr/cm2) than at 2.0 m depth (0.2920.030 mg O2/hr/g fr wt or 0.4260.135 g O2/hr/cm

    2). Respiration

    rate was not significantly difference at the two depths. Laboratory study showed that the rate of photosynthesis varied with

    light intensity, exhibiting saturation at 200-800 mol/m2/sec with a light compensation point at 20-40 mol/m2/sec. The

    in situ light measurement recorded at 2.0 m depth was 108.339.18 mol/m2/sec, which is comparatively higher than those

    at compensation light point, which suggests that this seagrass may inhabit the depth more than 2.0 m. However, based on

    field observation, this seagrass was only found at depth of 1.5-2.0 m HWL.

    Seagrass is a productive component in shallow marine

    ecosystems that contribute significantly to the coastal

    water carbon balance1. In many coastal areas,

    seagrasses form extensive meadows, and are

    recognised to be important in stabilising sea floor2.

    The growth, distribution and abundance of seagrasses

    are influenced by current regime3, nutrient

    availability4, light intensity5, water temperature6 and

    salinity ranges7 where they are growing. The seagrassbiomass generally decreases with increasing depth

    due to light attenuation and the vertical distribution of

    different seagrasses also depends on different light

    intensity9,10.

    The seagrass bed of Batu Tujuh (Port Dickson),

    which consists seven of the 13 seagrass species

    reported from Malaysia11,12 are distributed along a

    depth gradient ranging from intertidal zone down to

    about 6 m. Among the seven seagrasses, C. serrulata

    (Magnoliophyta/Potamogetonales/ Cymodoceaceae)

    grows in intertidal area and never found in deeper

    area with Halophila decipiens and big leavesvariantHalophila ovalis in this seagrass bed12. Therefore, it is

    assumed that light availability is a contributing factor

    that controls the penetration ofC. serrulata in deeper

    area in this seagrass bed. Hence, this study was

    undertaken to detect the rate of photosynthesis ofC.

    serrulata at different depths and the adaptational

    responses of this seagrass to different light intensities.

    This study will reveal the possible contribution of

    light on this intertidal species in one of the seagrass

    bed at Port Dickson, Malaysia.

    The present study was conducted at Port Dickson,

    Negeri Sembilan, Malaysia. It is an inshore tidal area

    along the straits of Malacca (lat. 2 27 N ; long. 101

    51 E). Presently, in situ photosynthesis study at

    different depths was conducted under natural lightintensity from 1100 to 1400 hrs. Shoots of seagrass of

    this species were collected and placed in the glass

    cylinder (30 cm height, 2.6 cm diameter) filled with

    seawater. The mouths of cylinder were closed with

    rubber stopper ensuring that no air bubble was

    present. Some of the cylinders were wrapped with

    aluminium foil to generate the dark condition for dark

    respiration. Ambient seawater was used for both light

    and dark bottle experiments. Three replicates were

    used at each depth for both photosynthesis and

    respiration measurement. Other glass cylinders were

    used as blanks including seawater without plants todetect the water photosynthesis and respiration by

    phytoplankton and bacteria. All cylinders were

    incubated for 3 h at 0.5 m and 2.0 m depth of

    seawater. After incubation for 3 h, the oxygen

    produced or consumed was detected by oxygen

    electrode methods (Rank Brothers Limited, UK). The

    light intensity was determined by using a light sensor

    (LICOR, Model 189). For the light response of

    photosynthesis study, experiment was carried out in

    the laboratory immediately after collection of

    *Corresponding authorE mail: [email protected]

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    INDIAN J MAR. SCI., VOL. 30, No. 4, DECEMBER 2001254

    specimens. The rate of photosynthesis was determined

    as O2 evolution13. About 1.5 to 2.0 cm long leaf

    segment was placed in the cuvet chamber. Three

    replicates were used for this detection and the mean

    value was used. The photosynthesis measurement wascarried out at 28C with the light source provided by

    250 watt halogen lamp. Light intensity (20 - 1600

    mol/m2/sec) was varied by adjusting the distance of

    light source from the chamber. Total chlorophyll

    content was measured by the procedure described by

    Arnon14.

    Photosynthesis is a process of energy fixation that

    is strongly affected by environmental factors,

    temperature and light intensity. The rate of

    photosynthesis of C. serrulata was higher at 0.5 m

    than at 2 m (Fig. 1). This difference could be

    attributed to higher light intensity at the depth of 0.5m than 2 m (Fig. 2). However, the reduction of

    photosynthesis at 2 m depth was not consistent with

    the light attenuation. The light attenuation was almost

    linear (y = -132.33x+363.46, r2 = 0.974, P < 0.05)

    with the depth to 2 m below the water surface. The

    light intensity at 2 m reduced to around 72% of the

    light at 1 m. However, the photosynthetic rate at 2 m

    reduced only by about 39% (based on fr wt) or 26%

    (based on leaf area). This could possibly be due to

    difference in light quality at various depths as a result

    of light absorption by water molecule and various

    suspended matter in the water body. Since samples

    used in the experiment were collected from the samelocality, the variation in sample could be ruled out.

    In contrast, respiration rates for both fresh leaf

    tissue and leaf surface area of this species were not

    significantly different (t-test, P > 0.05) between the

    two depths (Fig. 1). Respiration remains

    approximately the same provided that temperature

    and other factors are essentially unchanged15, which

    support the present finding. The normal oxygen

    requirement for respiration ofC. serrulata was almost

    equal to theHalophila stipulacea (0.20 mgO2/hr/g dry

    weight16. The respiration rates for other seagrasses

    Halophila ovalis and Halodule uninervis were0.920.13 and 0.340.13 mgO2/hr/g dry weight,

    respectively16, with a much oxygen requirement when

    compared to C. serrulata.In laboratory study of C. serrulata, the maximum

    photosynthetic rate recorded was 39.869.57 gO2/min/g fr wt, 0.0620.02 g O2/min/cm

    2 leaf areaor 40.946.54 g O2/min/mg chlorophyll at the lightintensity of 800 mol/m2/sec (Fig. 3). No netphotosynthesis was observed at 20 and 40mol/m2/sec. Photosynthetic rates decreasedgradually when the light intensity increased above800 mol/m2/sec. The light compensation of

    C. serrulata was at the light intensity of 20-40 mol/m2/sec. Clarke15 stated that at light intensities belowthis value, photosynthesis may still go on but the plantcannot survive because the energy lost due to theactivities of catabolic process represented byrespiration, which exceed the gain in energy, brought

    Fig. 1Photosynthesis and respiration rate at 0.5 and 2.0 m

    depths of seagrass Cymodocea serrulataA) based on fresh

    weight, B) based on leaf surface area

    Fig. 2Light intensity of different depths during the experimentaltime (July 10, 1999) of seagrass Cymodocea serrulata of Batu

    Tujuh seagrass bed, Teluk Kemang, Port Dickson.

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    SHORT COMMUNICATION 255

    by the anabolic process of photosynthesis. The lightcompensation of the present study was comparablewith the values of other seagrass reported byDennison9 and Bulthuis17. Pollard & Greenway18found that high light compensation for Cymodoceaserrulata, Thalassia hemprichii and Zosteracapricorni were due to high respiration demand of theplants, which resulted from the high watertemperature. They also found that the lightcompensation points were 80 to 98 mol/m2/sec dueto high water temperature (29-33C) in Australianseagrass beds. In present experiment the temperaturewas 28C throughout the experimental period.

    The light response of seagrass C. serrulata showed

    increased photosynthesis correspondingly with the

    light intensity from 40 to 200 mol/m2/sec and

    photosynthesis peaked at light saturation at 200-800

    mol/m2/sec. The photosynthesis irradiance (PI)

    curve relation revealed that photoinhibition was set

    when the light intensity increased beyond

    800 mol/m2/sec forC. serrulata. The light intensity

    at 1 cm below the surface during the study period was

    around 370 mol/m2/sec. This is far below the

    minimum intensity that may cause photoinhibition. It

    is predicted that based on laboratory experiments,

    C. serrulata is capable to carry out photosynthesis atvery shallow water such as low tide, as well as below

    2 m depth. On the other hand, this seagrass could also

    penetrate deeper area with Halophila decipiens and

    big leaves variant Halophila ovalis in this study

    area12. However, in the present study area the limited

    intertidal distribution of C. serrulata could possibly

    be affected by other environmental factors i.e.

    substratum, current movement or other factors.

    Authors are grateful to Malaysian Government for

    financial support (IRPA) project no. 08-02-04-019.

    References1 McRoy C P & McMillan C, Production ecology and

    physiology of seagrass, in Seagrass ecosystems: A scientificperspective, edited by C P McRoy & C Helfferich, (MarcelDekker, New York, Basel) 1977, pp. 53-87.

    2 Fonseca M S & Fisher J S, A comparison of canopy frictionand sediment movement between four species of seagrasswith reference to their ecology and restoration, Mar EcolProg Ser, 29 (1986) 15-22.

    3 Fonseca M S & Kenworthy W J, Effects of current onphotosynthesis and distribution of seagrasses, Aquat Bot, 27(1987) 59-78.

    4 Short F T, Effects of sediment nutrients on seagrass:Literature review and mesocosm experiment, Aquat Bot, 27(1987) 41-57.

    5 Dennison W C & Alberte R S, Photosynthetic responses ofZostera marina L. (eelgrass) to in situ manipulations of lightintensity, Oecologia, 55 (1982) 137-140.

    6 Bulthuis D A, Effects of temperature on photosynthesis andgrowth of seagrass,Aquat Bot, 27 (1987) 27-40.

    7 Walker D I & McComb A J, Salinity response of the seagrassAmphibolis antarctica (Labill.) Sonder ex Aschers: Anexperimental validation of field results, Aquat Bot, 36 (1990)359-366.

    8 Bulthuis D A & Woelkerling W M J, Effects of in situnitrogen and phosphorus enrichment of the sediments on the

    seagrass Heterozostera tasmanica (Mart. Ex Aschers.) den

    Hartog in Western Port, Victoria, Australia, J Exp Biol &

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    9 Dennison W C, Effects of light on seagrass photosynthesis,growth and depth distribution,Aquat Bot, 27 (1987) 15-26.

    10 Dawes C J & Tomasko D A, Depth distribution ofThalassiatestudinum in two meadows on the West Coast of Florida: A

    difference in effect of light availability, Mar Ecol, 9 (1988)

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    11 Japar Sidik B, Arshad A & Law A T, Inventory for seagrassbeds in Malaysia. Malaysian inventory of coastal watersheds,

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    Fig. 3Photosynthesis rate of seagrass Cymodocea serrulata at

    different light intensities,A) based on fresh weight, B) based onleaf surface area, C) based on chlorophyll content

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    INDIAN J MAR. SCI., VOL. 30, No. 4, DECEMBER 2001256

    12 Lee C N, Seagrass and macroalgal communities in theintertidal and subtidal waters of Teluk Kemang, 7

    thmile Port

    Dickson, BSc Project Paper (Department of Biology,Universiti Putra Malaysia) 1999, pp. 146.

    13 Walker D, The use of the oxygen electrode and fluorescenceprobes in simple measurements of photosynthesis,(Oxygraphics Limited, London, UK) 1988, pp. 203.

    14 Arnon D I, Copper enzymes in isolated chloroplastpolyphenoloxidase inBeta vulgaris, Plant Physiol, 24 (1949)1-15.

    15 Clark G L,Elements of ecology, (John Wiley, London) 1967,pp. 560.

    16 Wahbeh M I, Productivity and respiration of three seagrassspecies from the Gulf of Aqaba (Jordan) and some relatedfactors,Aquat Bot, 15 (1983) 367-374.

    17 Bulthuis D A, Effects of temperature on the photosynthesis-irradiance of the Australian seagrass Heterozostera

    tasmanica, Mar Bio Lett, 4 (1983) 47-57.18 Pollard P C & Greenway M, Photosynthesis characteristic ofseagrass (Cymodocea serrulata, Thalassia hemprichii and

    Zostera capricorni) in a low light environment, with acomparison of leaf marking and lacunal gas measurements of

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    127- 139.