The marine coccolithophorid Emiliania huxleyi is a cosmopolitan alga intensely studied in relation to global carbon cycling, biogeochemistry, marine ecology, and biomineralization processes. The biomineralization capabilities of coccolithophorids have attracted the attention of scientists interested in exploiting this ability for the development of materials science and biomedical and biotechnological applications. Although it has been well documented that biomineralization in E. huxleyi is promoted by growth under phosphate-limited conditions, the genes and proteins that govern the processes of calcification and coccolithogenesis remain unknown. Suppressive subtractive hybridization (SSH) libraries were constructed from cultures grown in phosphate-limited and phosphate-replete media as tester and driver populations for reciprocal SSH procedures. Positive clones from each of the two libraries were randomly selected, and dot blotting was performed for the analysis of expression patterns. A total of 513 clones from the phosphate-replete library and 423 clones from the phosphate-limited library were sequenced, assembled, and compared to sequences in GenBank using BLASTX. Of the 103 differentially expressed gene fragments from the phosphate-replete library, 34% showed significant homology to other known proteins, while only 23% of the 65 differentially expressed gene fragments from the phosphate-limited library showed homology to other proteins. To further assess mRNA expression, real-time RT-PCR analysis was employed and expression profiles were generated over a 14-day time course for three clones from the phosphate-replete library and five clones from the phosphate-limited library. The fragments isolated provide the basis for future cloning of full-length genes and functional analysis.Coccolithophorids are unicellular marine algae that produce a wide variety of highly sculpted calcium carbonate cell coverings. Calcification in some coccolithophorids occurs intracellularly and is thought to begin with the conversion of calcium and bicarbonate ions into crystals of calcium carbonate that are deposited in a defined array in association with an organic matrix (35). A coccolith vesicle developing from the Golgi apparatus provides the microenvironment that promotes the formation of the crystallographically intricate coccolith structures, which are subsequently extruded from the cell to form the coccosphere (7,20). The coccolith vesicle fuses with the plasma membrane to release the individual coccoliths. While calcification and coccolithogenesis are presumed to occur in a genetically controlled manner, the functional significance and genetic control of these complex structures and the variation in crystal shape, orientation, order, and connectivity that occurs across species are poorly understood The size and morphology of the calcite structures are as diverse as the coccolithophorids that produce them. Some of the calcite elements are simple rhombohedral units, while others appear as ornate oval platelets, extended spic...