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海洋潮间带环境中的氧气和二氧化碳:岩池中的昼夜和潮汐变化

Oxygen and carbon dioxide in the marine intertidal environment: diurnal and tidal changes in rockpools.

作者信息

Truchot J P, Duhamel-Jouve A

出版信息

Respir Physiol. 1980 Mar;39(3):241-54. doi: 10.1016/0034-5687(80)90056-0.

Abstract

Water oxygen partial pressure (PO2), pH, titration alkalinity (TA), temperature and salinity were measured hourly in rockpools during emersion periods occuring at various times of the diurnal cycle. Measurements allowed calculation of oxygen concentration (CO2), CO2 partial pressure (PCO2) and concentrations of bicarbonate, carbonate and total CO2 (CCO2). During night emersion periods, water PO2 decreased to almost zero in a few hours, pH fell, TA rose and PCO2 increased up to 1-3 Torr. During day emersion periods, water PO2 rose to 400-600 Torr, pH increased to more than 10, TA decreased substantially and PCO2 fell as low as 10(-4) Torr. The direction of the observed changes depended essentially on the illumination, indicating that respiratory and photosynthetic activities were the main processes involved. The large variations of the components of the carbonate system imply considerable changes of the CO2 capacitance coefficient in water, mainly during the day-time emersion. These changes are discussed in relation to the respiratory and acid-base physiology of the animals living in these biotopes.

摘要

在昼夜循环不同时间出现的干露期,每小时测量岩池中水体的氧分压(PO2)、pH值、滴定碱度(TA)、温度和盐度。通过这些测量可以计算出氧浓度(CO2)、二氧化碳分压(PCO2)以及碳酸氢盐、碳酸盐和总二氧化碳(CCO2)的浓度。在夜间干露期,水体PO2在数小时内降至几乎为零,pH值下降,TA升高,PCO2升高至1 - 3托。在白天干露期,水体PO2升至400 - 600托,pH值升至10以上,TA大幅下降,PCO2降至低至10^(-4)托。观察到的变化方向主要取决于光照,这表明呼吸和光合活动是主要相关过程。碳酸盐系统各成分的大幅变化意味着水体中二氧化碳电容系数有相当大的变化,主要在白天干露期间。结合生活在这些生物群落中的动物的呼吸和酸碱生理学对这些变化进行了讨论。

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