Pigments as markers of processes
The pheophorbides (these are the Chlorophyll molecules without Mg ion and phytol chain) arise when a Chlorophyll-a containing particle passes through the digestive tract of meso and makrozooplankton. Therefore, the ratio of pheophorbides to intact Chlorophyll-a in the water column can offer an idea of the grazing pressure experienced by phytoplankton community. The same ratio, determined in sunken material shows the influence of feces on sedimentation.
On the use of the degradation products of Carotenoids, and Phycobilins in this context is still little known.
Which main questions can be answered by pigment analysis?
1. Which classes of phytoplankton are involved in the composition of a given community and how much does each class contribute to total Chlorophyll-a?
2. How do the communities change over time?
3. Are there differences in the vertical distribution of the classes?
4. What classes contribute how much to the vertical flux?
5. What influence has the feeding activity of the zooplankton on phytoplankton communities and their decline?
6. Are there feeding preferences of zooplankton in relation to individual phytoplankton classes?
Literature cited:
MACKEY, M.D., D.J. MACKEY, H.W. HIGGINS and S.W. WRIGHT (1996) CHEMTAX ‑ a program for estimating class abundances from chemical markers: application to HPLC measurements of phytoplankton. Mar. Ecol. Prog. Ser. 144: 265‑283