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                        Box 9.10  Atomic force microscopy of coccolithophores

               Coccolithophores, despite their small size, are attractive and sophisticated organisms. A number of
               plate morphs, emphasizing the diversity of form within the group, have been described (Fig. 9.18c):
               asterolith, star-shaped plates; cyclolith, open rings; lopadolith, vase-shaped morphs with elevated
               edges; placolith, two disks fused by the median tube; stetolith, column-shaped plates; zygolith, ellipti-
               cal ring with arches applied to holococcoliths. Apart from the term placolith most are not in routine
               use. Additionally, helioliths, composed of a large number of small radially arranged crystals, and
               ortholiths, with only a few crystals, have been recognized.
                  The coccolithophore is precipitated within the cell from the coccolith vesicle or Golgi body with
               tightly regulated crystal growth, allowing the crystals to integrate as the complex and exquisite net-
               works that comprise a complete skeleton. Karen Henriksen, a former graduate student at the Uni-
               versity of Copenhagen, applied atomic force microscopy (AFM) to the surface of three coccolith
               species, a technique that allows investigation at higher orders of magnitude than even scanning
               electron microscopy (SEM) and transmission electron microscopy (TEM) equipment. Henriksen and
               colleagues (2004) established key differences among these taxa suggesting that subtle changes in the

               mechanisms of biomineralization can drive significant changes in morphology that have knock-on
               effects for the adaptability, lifestyle and distribution of the coccolith species. The large morphological
               disparity seen in this remarkable group is thus a function of the mode and orientation of crystal
               growth at the atomic level and where the organism ultimately lived depended on the whims of a
               crystal lattice.




             they then migrate to the cell surface and are   flagellate, and is usually coated by minute
             expelled to form a composite exoskeleton, the   holococcoliths; the  diploid  phase  (with full
             coccosphere. Commonly the coccosphere           complement of chromosomes) is usually non-
             consists of 10–30 discrete coccoliths, although   flagellate, and is coated by heterococcoliths.

             some forms have many more (Box 9.10).           Both phases are capable of indefi nite asexual
             Many taxa produce coccospheres formed of        reproduction and it appears likely that the
             only one type of coccolith, but others show a   two-phase life cycle is an adaptation allowing
             variety of coccolith morphologies (Fig. 9.18);   coccolithophores to survive challenging eco-
             in particular there are often specialized coc-  logical conditions. The haploid (holoccolith-
             coliths around the flagellar pole of the cell.   producing) phase is thought to be adapted to

             There are two fundamentally different types     oligotrophic conditions (when nutrients are
             of coccoliths: heterococcoliths have a radial   scarce) whilst the diploid (heterococcolith-
             array of relatively few (typically 20–50)       producing) phase is thought to be adapted to
             complex-shaped crystal units, whereas holo-     more eutrophic conditions (when nutrients
             coccoliths are formed of planar arrays of hun-  are abundant).

             dreds of minute uniform-sized (typically c.       The classification of extant coccolitho-
             0.1 μm) rhombohedral crystallites.              phores is based largely on coccosphere mor-
               Haptophyte life cycles were very poorly       phology and coccolith structure because the
             known until recently; research has now shown    intricate and distinctive form of coccoliths
             that cocolithophores, and possibly most hap-    makes them ideal for morphological classifi -
             tophtes, typically have alternating haploid     cation. Cell characters can only be studied
             and diploid stages that are both capable        with transmission electron microscopy and
             of asexual reproduction. Coccolithophores       have generally proved rather invariant. Data
             usually have life cycles consisting of two main   from cytology and molecular genetics have
             phases producing radically different cocco-     strongly supported the classifi cation based on
             liths that were often described initially as two   morphological criteria. The reliance on coc-
             different species. The haploid phase (with half   coliths in the extant classifi cation also means
             the complement of chromosomes) is always        that there are relatively few problems in align-
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