scholarly journals Variation of seawater temperature and chlorophyll-a prior to and during upwelling event in Bali Strait, Indonesia: from observation and model

Author(s):  
W E Rintaka ◽  
B Priyono
Sensors ◽  
2020 ◽  
Vol 20 (19) ◽  
pp. 5471
Author(s):  
Lina Cai ◽  
Juan Bu ◽  
Danling Tang ◽  
Minrui Zhou ◽  
Ru Yao ◽  
...  

We analyzed the distribution of chlorophyll-a (Chla) in the Bohai Sea area based on data from the geosynchronous orbit optical satellite Gaofen-4 (GF-4), which was launched in 2015, carrying a panchromatic multispectral sensor (PMS). This is the first time the geosynchronous orbit optical satellite GF-4 remote-sensing data has been used in China to detect the Chla change details in the Bohai Sea. A new GF-4 retrieved model was established based on the relationship between in situ Chla value and the reflectance combination of 2 and 4 bands, with the R2 of 0.9685 and the total average relative error of 37.42%. Twenty PMS images obtained from 2017 to 2019 were applied to analyze Chla in Bohai sea. The results show that: (1) the new built Chla inversion model PMS-1 for the GF-4 PMS sensor can extract Chla distribution details in the Bohai Sea well. The high Chla content in the Bohai Sea is mainly located in coastal areas, such as the top of Laizhou Bay, Bohai Bay and Liaodong Bay, with the value being around 13 µg/L. The concentration of Chla in the Bohai Strait and northern Yellow Sea is relatively low with the value being around 5 µg/L. (2). Taking full advantage of the continuous observation of geostationary orbit satellite, GF-4 with a high-resolution sensor PMS of 50 m can effectively detect short-term change (changes within 10 min) in Chla concentration. The changes mainly appear at the southwest and northeast costal area as well as in the center of Bohai Sea with the change value of around 3 µg/L. (3) The change of Chla concentration in the Bohai sea is related to the environmental factors such as seawater temperature, salinity, illumination and nutrient salts, as well as the dynamic factors such as wind, flow field and tidal current.


2021 ◽  
Vol 49 (4) ◽  
pp. 640-648
Author(s):  
Pamela González ◽  
Armando Mujica ◽  
María Luisa Nava

Euphausia mucronata abundance and distribution of the developmental stages (calyptopis, furciliae, juveniles, and adults) was analyzed as a function of seawater temperature and chlorophyll-a concentration between Paposo (25°S) and Coquimbo (30°S), Chile. Zooplankton samples were obtained using bongo nets during February of three consecutive years (2014-2016). The Q coefficient was used to explore the relationship between the distribution and abundance of the development stages of E. mucronata with the temperature recorded throughout the water column. The adults were considerably more abundant than the rest of the ontogenetic development stages during the study period. The abundance of adults decreased from February 2014 to 2016, having a negative correlation with temperature. Relative abundance of juveniles and larvae increased positively related to the total euphausiid abundance. The Q coefficient showed a significant association of all development states concerning the low-temperature intervals recorded throughout the seawater column. Q coefficient showed no association with chlorophyll-a concentration through the recorded intervals throughout the water column and neither with the vertical abundance and distribution of E. mucronata specimens.


2021 ◽  
Vol 944 (1) ◽  
pp. 012055
Author(s):  
A Suprianto ◽  
A S Atmadipoera ◽  
J Lumban-Gaol

Abstract Bali Strait is part of fisheries management zone (WPP 573), where abundant fishery potential, of lemuru fish commodity. Here, physical oceanographic setting such as upwelling event plays an important role on maintaining high primary productivity and lemuru fish distribution. This study aims to describe physical process and dynamics of seasonal coastal upwelling using time-series datasets (2008 and 2014) of temperature, salinity, current velocity, surface chlorophyll-a (chl-a) from INDESO model and satellite imagery. The results showed that upwelling in the Bali Strait only during the southeast monsoon period when the south-easterly wind force surface Ekman drift of about 5.5 × 10−3 Sv flowing south-eastward (toward offshore). Upwelling event is characterized by minimum parameter of sea surface temperature (24.93 °C), and sea level anomaly (0.75 m), but maximum of surface chlorophyll-a (1.33 mg/m3). Furthermore, isotherm of 26 °C and Isohaline 33.7 psu are outcropped at sea surface in the center of upwelling zone. In contrast, during the nortwest monsoon period these isolines remain at deeper layer of about 80-90 m depth. Mean temperature-based upwelling index during peak of upwelling in August (1.19±0.19 °C). Upwelling impact on high abundance of lemuru fish (Sardinella sp.) production two month later after peak of chl-a.


2021 ◽  
Author(s):  
◽  
Łukasz Stefan Lachowicz

<p>This study examines the population ecology and dynamics of three co-existing mussel species (Aulacomya maoriana, Mytilus galloprovincialis and Perna canaliculus) in Wellington Harbour, New Zealand. The present study investigates the role of multiple environmental factors and their multiple effects on the intertidal mussel population. Wellington Harbour is a complex system, supporting speciose intertidal invertebrate communities. CTD data loggers recording seawater temperature, turbidity, chlorophyll a concentration and salinity at Evans Bay, Seatoun, Matiu-Somes Island and Petone provided the environmental data. The data suggest the existence of distinct zones within Wellington Harbour, with different hydrological regimes present at each zone. Consistently high salinity (35.08 + 2.9 PSU) and chlorophyll a concentration (9.42 + 4.33 μg l-1) were found at Evans Bay, while these parameters displayed a degree of temporal variation and were significantly lower at Seatoun (31.5 + 4.17 PSU and 2.15 + 2.1 μg l-1) and Matiu-Somes Island (33.26 + 0.99 PSU and 1.23 + 1.79 μg l-1). At Petone, a site located near the Hutt river mouth, salinities were reduced (31.59 + 3.21 PSU) while chlorophyll a levels were similar to those at Matiu-Somes Island (1.64 + 1.08 μg l-1). Mean turbidity values were similar at Seatoun and Evans Bay (11.51 + 18.53 FTU and 11.89 + 5.52 FTU, respectively), with mean turbidity slightly reduced at Petone (8.20 + 11.16 FTU) and elevated at Matiu-Somes Island (15.35 + 11.12 FTU). Further, CTD data revealed similar seawater temperature at all sites, with mean values oscillating around 13 - 15ºC. The ecology of larval stages was expressed in this study by quantifying the rates at which mussel larvae settled on the experimental substrate. A year-round spawning, as well as temporal and spatial variability in mussel recruitment at four experimental sites was revealed. Evans Bay was the site with consistently higher recruitment rates but not the mean recruit numbers (721 + 879 larvae), while the highest number of recruits (9851 larvae) was recorded at Petone (1041 + 2112 larvae). Recruitment rates were lower at Seatoun (729 + 536 larvae) and Matiu-Somes Island (410 + 636 larvae). However, only at Seatoun was this variability clearly linked to the environmental conditions of water turbidity, chlorophyll a concentration, and salinity. The post-larval ecology part of this study concentrates on the condition index and gonad mass, and the degree of infestation with a parasitic pea crab Pinnotheres novaezelandiae studied at four sites. Spatial and temporal variation in condition index and gonad mass was revealed in all three species investigated, with both condition index and gonad mass of adult mussels being highest at Matiu-Somes Island (14.59 + 4.41 and 0.21 + 0.16 g), followed by Kau Point (13.47 + 6.99 and 0.17 + 0.10 g), Seatoun (13.32 + 7.79 and 0.11 + 0.10 g) and Evans Bay (11.99 + 2.78 and 0.14 + 0.14 g). Condition index was significantly correlated with gonad mass, and was highest in Aulacomya maoriana (15.85 + 9.38), followed by Perna canaliculus (12.52 + 4.39) and Mytilus galloprovincialis (11.66 + 5.91). The condition was generally reduced in mussels infested with the pea crab Pinnotheres novaezelandiae, although the overall infestation rate was low (3.28%). In order to describe the pattern of mussel community development, patches of bare rock were experimentally created in the mid-intertidal zone. Subsequently, predatorexclusion cages were set up in those areas and monitored regularly. The abundance of main groups of intertidal taxa settling on the cleared substrate was expressed in terms of percent cover, and was highest at Evans Bay (59.57 + 80.27%), lowest at Kau Point (13.96 + 26.18%) and intermediate at Seatoun (22.56 + 41.64%). However, the bottomup factors were visibly linked to the community development at Seatoun. The full cage experimental treatment provided the maximum protection from predation and desiccation, therefore the community recovery was most pronounced under this treatment. Mytilus galloprovincialis was revealed as the most competitive mussel species, in some cases able to colonise the entire available substrate and exclude other two mussel species. Further, seasonality of mussel response to wave action and desiccation was investigated. Mussel species-specific strength of attachment to the rocky substrate was expressed in kg (effectively the force) required for the mussel to be removed from the rocky substrate at shores facing south and north in Wellington Harbour. The strength of attachment was highest in Perna canaliculus (5.81 kg + 2.27), followed by Aulacomya maoriana (3.63 kg + 1.63) and Mytilus galloprovincialis (3.44 kg + 1.70). Mussel strength of attachment was generally higher at south-facing sites, due to stronger waves generated by southerly winds. In a separate experiment, in which mussels were exposed to air at six different shore levels within the intertidal zone, desiccation tolerance was highest in Mytilus galloprovincialis on the south-facing sites (LD50=0.62m and 0.87 for north- and south-facing sites, respectively), followed by Aulacomya maoriana (LD50=0.65 and 0.75m for north- and south-facing sites, respectively) and Perna canaliculus (LD50=0.20 and 0.35m for north- and south-facing sites, respectively). LD50 desiccation exposure values were lower in all three species found on the north-facing shores, indicating that mussels on those shores are less tolerant to desiccation-induced stress and therefore died more rapidly.</p>


2021 ◽  
Author(s):  
◽  
Łukasz Stefan Lachowicz

<p>This study examines the population ecology and dynamics of three co-existing mussel species (Aulacomya maoriana, Mytilus galloprovincialis and Perna canaliculus) in Wellington Harbour, New Zealand. The present study investigates the role of multiple environmental factors and their multiple effects on the intertidal mussel population. Wellington Harbour is a complex system, supporting speciose intertidal invertebrate communities. CTD data loggers recording seawater temperature, turbidity, chlorophyll a concentration and salinity at Evans Bay, Seatoun, Matiu-Somes Island and Petone provided the environmental data. The data suggest the existence of distinct zones within Wellington Harbour, with different hydrological regimes present at each zone. Consistently high salinity (35.08 + 2.9 PSU) and chlorophyll a concentration (9.42 + 4.33 μg l-1) were found at Evans Bay, while these parameters displayed a degree of temporal variation and were significantly lower at Seatoun (31.5 + 4.17 PSU and 2.15 + 2.1 μg l-1) and Matiu-Somes Island (33.26 + 0.99 PSU and 1.23 + 1.79 μg l-1). At Petone, a site located near the Hutt river mouth, salinities were reduced (31.59 + 3.21 PSU) while chlorophyll a levels were similar to those at Matiu-Somes Island (1.64 + 1.08 μg l-1). Mean turbidity values were similar at Seatoun and Evans Bay (11.51 + 18.53 FTU and 11.89 + 5.52 FTU, respectively), with mean turbidity slightly reduced at Petone (8.20 + 11.16 FTU) and elevated at Matiu-Somes Island (15.35 + 11.12 FTU). Further, CTD data revealed similar seawater temperature at all sites, with mean values oscillating around 13 - 15ºC. The ecology of larval stages was expressed in this study by quantifying the rates at which mussel larvae settled on the experimental substrate. A year-round spawning, as well as temporal and spatial variability in mussel recruitment at four experimental sites was revealed. Evans Bay was the site with consistently higher recruitment rates but not the mean recruit numbers (721 + 879 larvae), while the highest number of recruits (9851 larvae) was recorded at Petone (1041 + 2112 larvae). Recruitment rates were lower at Seatoun (729 + 536 larvae) and Matiu-Somes Island (410 + 636 larvae). However, only at Seatoun was this variability clearly linked to the environmental conditions of water turbidity, chlorophyll a concentration, and salinity. The post-larval ecology part of this study concentrates on the condition index and gonad mass, and the degree of infestation with a parasitic pea crab Pinnotheres novaezelandiae studied at four sites. Spatial and temporal variation in condition index and gonad mass was revealed in all three species investigated, with both condition index and gonad mass of adult mussels being highest at Matiu-Somes Island (14.59 + 4.41 and 0.21 + 0.16 g), followed by Kau Point (13.47 + 6.99 and 0.17 + 0.10 g), Seatoun (13.32 + 7.79 and 0.11 + 0.10 g) and Evans Bay (11.99 + 2.78 and 0.14 + 0.14 g). Condition index was significantly correlated with gonad mass, and was highest in Aulacomya maoriana (15.85 + 9.38), followed by Perna canaliculus (12.52 + 4.39) and Mytilus galloprovincialis (11.66 + 5.91). The condition was generally reduced in mussels infested with the pea crab Pinnotheres novaezelandiae, although the overall infestation rate was low (3.28%). In order to describe the pattern of mussel community development, patches of bare rock were experimentally created in the mid-intertidal zone. Subsequently, predatorexclusion cages were set up in those areas and monitored regularly. The abundance of main groups of intertidal taxa settling on the cleared substrate was expressed in terms of percent cover, and was highest at Evans Bay (59.57 + 80.27%), lowest at Kau Point (13.96 + 26.18%) and intermediate at Seatoun (22.56 + 41.64%). However, the bottomup factors were visibly linked to the community development at Seatoun. The full cage experimental treatment provided the maximum protection from predation and desiccation, therefore the community recovery was most pronounced under this treatment. Mytilus galloprovincialis was revealed as the most competitive mussel species, in some cases able to colonise the entire available substrate and exclude other two mussel species. Further, seasonality of mussel response to wave action and desiccation was investigated. Mussel species-specific strength of attachment to the rocky substrate was expressed in kg (effectively the force) required for the mussel to be removed from the rocky substrate at shores facing south and north in Wellington Harbour. The strength of attachment was highest in Perna canaliculus (5.81 kg + 2.27), followed by Aulacomya maoriana (3.63 kg + 1.63) and Mytilus galloprovincialis (3.44 kg + 1.70). Mussel strength of attachment was generally higher at south-facing sites, due to stronger waves generated by southerly winds. In a separate experiment, in which mussels were exposed to air at six different shore levels within the intertidal zone, desiccation tolerance was highest in Mytilus galloprovincialis on the south-facing sites (LD50=0.62m and 0.87 for north- and south-facing sites, respectively), followed by Aulacomya maoriana (LD50=0.65 and 0.75m for north- and south-facing sites, respectively) and Perna canaliculus (LD50=0.20 and 0.35m for north- and south-facing sites, respectively). LD50 desiccation exposure values were lower in all three species found on the north-facing shores, indicating that mussels on those shores are less tolerant to desiccation-induced stress and therefore died more rapidly.</p>


2013 ◽  
Vol 10 (10) ◽  
pp. 15559-15586
Author(s):  
M. N. Müller ◽  
M. Lebrato ◽  
U. Riebesell ◽  
J. Barcelos e Ramos ◽  
K. G. Schulz ◽  
...  

Abstract. Marine calcareous sediments provide a fundamental basis for paleoceanographic studies aiming to reconstruct past oceanic conditions and understand key biogeochemical element cycles. Calcifying unicellular phytoplankton (coccolithophores) are a major contributor to both carbon and calcium cycling by photosynthesis and the production of calcite (coccoliths) in the euphotic zone and the subsequent long-term deposition and burial into marine sediments. Here we present data from controlled laboratory experiments on four coccolithophore species and elucidate the relation between the divalent cation (Sr, Mg and Ca) partitioning in coccoliths and cellular physiology (growth, calcification and photosynthesis). Coccolithophores were cultured under different seawater temperature and carbonate chemistry conditions. The partition coefficient of strontium (DSr) was positively correlated with both carbon dioxide (pCO2) and temperature but displayed no coherent relation to particulate organic and inorganic carbon production rates. Furthermore, DSr correlated positively with cellular growth rates when driven by temperature but no correlation was present when changes in growth rates were pCO2-induced. The results demonstrate the complex interaction between environmental forcing and physiological control on the strontium partitioning in coccolithophore calcite. The partition coefficient of magnesium (DMg) displayed species-specific differences and elevated values under nutrient limitation. No conclusive correlation between coccolith DMg and temperature was observed but pCO2 induced a rising trend in coccolith DMg. Interestingly, the best correlation was found between coccolith DMg and chlorophyll a production suggesting that chlorophyll a and calcite associated Mg originate from the same intracellular pool. These results give an extended insight into the driving factors that lead to variations in the coccolith Mg / Ca ratio and can be used for Sr / Ca and Mg / Ca paleoproxy calibration.


2014 ◽  
Vol 11 (4) ◽  
pp. 1065-1075 ◽  
Author(s):  
M. N. Müller ◽  
M. Lebrato ◽  
U. Riebesell ◽  
J. Barcelos e Ramos ◽  
K. G. Schulz ◽  
...  

Abstract. Marine calcareous sediments provide a fundamental basis for palaeoceanographic studies aiming to reconstruct past oceanic conditions and understand key biogeochemical element cycles. Calcifying unicellular phytoplankton (coccolithophores) are a major contributor to both carbon and calcium cycling by photosynthesis and the production of calcite (coccoliths) in the euphotic zone, and the subsequent long-term deposition and burial into marine sediments. Here we present data from controlled laboratory experiments on four coccolithophore species and elucidate the relation between the divalent cation (Sr, Mg and Ca) partitioning in coccoliths and cellular physiology (growth, calcification and photosynthesis). Coccolithophores were cultured under different seawater temperature and carbonate chemistry conditions. The partition coefficient of strontium (DSr) was positively correlated with both carbon dioxide (pCO2) and temperature but displayed no coherent relation to particulate organic and inorganic carbon production rates. Furthermore, DSr correlated positively with cellular growth rates when driven by temperature but no correlation was present when changes in growth rates were pCO2-induced. Our results demonstrate the complex interaction between environmental forcing and physiological control on the strontium partitioning in coccolithophore calcite and challenge interpretations of the coccolith Sr / Ca ratio from high-pCO2 environments (e.g. Palaeocene–Eocene thermal maximum). The partition coefficient of magnesium (DMg) displayed species-specific differences and elevated values under nutrient limitation. No conclusive correlation between coccolith DMg and temperature was observed but pCO2 induced a rising trend in coccolith DMg. Interestingly, the best correlation was found between coccolith DMg and chlorophyll a production, suggesting that chlorophyll a and calcite associated Mg originate from the same intracellular pool. These and previous findings indicate that Mg is transported into the cell and to the site of calcification via different pathways than Ca and Sr. Consequently, the coccolith Mg / Ca ratio should be decoupled from the seawater Mg / Ca ratio. This study gives an extended insight into the driving factors influencing the coccolith Mg / Ca ratio and should be considered for future palaeoproxy calibrations.


2013 ◽  
Vol 52 ◽  
pp. 133-149 ◽  
Author(s):  
Sara Cardeira ◽  
Filomena Rita ◽  
Paulo Relvas ◽  
Alexandra Cravo

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