Chlorophyll f
Chemical compound
From Wikipedia, the free encyclopedia
Chlorophyll f (Chl f) is a form of chlorophyll that absorbs further into the red (near-infrared light) spectrum than other chlorophylls. In 2010, it was reported by Min Chen to be present in stromatolites from Western Australia's Shark Bay.[2][3] It has been found in cyanobacteria inside deep caves which appear perfectly dark in the visible light spectrum, but are lit up in near-infrared light which reflects more effectively from the rocks, allowing the cyanobacteria to photosynthesize using light with a wavelength as long as 780nm.[4][5]
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| IUPAC name
[methyl 14-ethyl-8-formyl-4,13,18-trimethyl-20-oxo-3-{3-oxo-3-[(3,7,11,15-tetramethylhexadec-2-en-1-yl)oxy]propyl}-9-vinylphorbine-21-carboxylatato(2−)-κ4N23,N24,N25,N26]magnesium | |
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| Properties | |
| C55H70O6N4Mg[1] | |
| Molar mass | 907.4725 g/mol |
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
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The function of Chl f in photosynthetic reactions in plants and the wider ecological distribution of Chl f remains little studied. Chl f has been shown to support some of the roles in photosynthetic reactions, in both the energy transfer and in the charge separation processes.[6][7][8][9]
Chl f is produced from chlorophyllide f by chlorophyll synthase. Chlorophyllide f is made from chlorophyllide a by an enzyme known as PsbA4 or ChlF.[10]
