फाइटोप्लैंकटन हिंदी उपयोग और उदाहरण

"" ऊपरी प्रकाशित मण्डल सतह में ही प्राथमिक उत्पादक पौधे (हरे पौधे, पादप प्लवक (फाइटोप्लैंकटन) प्रकाश संश्लेषण द्वारा आहार उत्पन्न करते हैं) तथा प्राथमिक उपभोक्ता -जन्तुप्लवक (जूप्लैंकटन)- भी इसी मण्डल में रहते हैं तथा पादप प्लवक का सेवन करते हैं।

ऊपरी प्रकाशित मण्डल सतह में ही प्राथमिक उत्पादक पौधे (हरे पौधे, पादप प्लवक (फाइटोप्लैंकटन) प्रकाश संश्लेषण द्वारा आहार उत्पन्न करते हैं) तथा प्राथमिक उपभोक्ता -जन्तुप्लवक (जूप्लैंकटन)- भी इसी मण्डल में रहते हैं तथा पादप प्लवक का सेवन करते हैं।

फाइटोप्लैंकटन इसके अंग्रेजी अर्थ का उदाहरण

Though still categorized as the lowest, fifth category and not suitable for swimming, the water had less ammoniacal and nitrite compounds, and less algae while zooplankton Daphnia, which feeds on phytoplankton, reappeared in the lake.

American male voice actors Brassicasterol (24-methyl cholest-5,22-dien-3β-ol) is a 28-carbon sterol synthesised by several unicellular algae (phytoplankton) and some terrestrial plants, like rape.

The compensation depth between photosynthesis and respiration of phytoplankton in the ocean must be dependent on some factors: the illumination at the surface, the transparency of the water, the biological character of the plankton present, and the temperature.

A concern regarding the concept of the compensation point is it assumes that phytoplankton remain at a fixed depth throughout a 24-hour period (time frame in which compensation depth is measured), but phytoplankton experience displacement due to isopycnals moving them tens of meters.

The phytoplankton are followed by zooplankton.

This should be small enough to remove all zooplankton, most phytoplankton, and thus a large proportion of the cholera in the water (99%, according to laboratory studies).

It can be detected in the Redfield ratio or Redfield stoichiometry is the consistent atomic ratio of carbon, nitrogen and phosphorus found in marine phytoplankton and throughout the deep oceans.

While deviations from the canonical 106:16:1 ratio have been found depending on phytoplankton species and the study area, the Redfield ratio has remained an important reference to oceanographers studying nutrient limitation.

Redfield’s analysis of the empirical data led to him to discover that across and within the three oceans and Barents Sea, seawater had an N:P atomic ratio near 20:1 (later corrected to 16:1), and was very similar to the average N:P of phytoplankton.

Specifically, phytoplankton species with different N and P requirements compete within the same medium and come to reflect the nutrient composition of the seawater.

Considering that at the time little was known about the composition of “protoplasm", or the bulk composition of phytoplankton, Redfield did not attempt to explain why its N:P ratio should be approximately 16:1.

Redfield discovered the remarkable congruence between the chemistry of the deep ocean and the chemistry of living things such as phytoplankton in the surface ocean.

When nutrients are not limiting, the molar elemental ratio C:N:P in most phytoplankton is 106:16:1.