Girvanella and other algae as depth indicators

Girvarzella is interpreted to be the calcified sheath of a variety of filamentous blue‐green algae. At present there are no clear limits which can be set on its depth of occurrence. The usefulness of benthic calcareous algae as depth indicators in palaeoenvironmental studies is dependent upon the level of identification. At high taxonomic levels it is very limited. Algae are not restricted to the euphotic zone (ka. 150 m). Calcareous green algae are restricted to shallower water (0‐ca. 100 m) than are calcareous red algae (0‐ca. 400 m) but they are prone to fragmentation and subsequent transportation. Narrower depth limits for lower taxonomic levels have been demonstrated in Recent green and red algae, but have yet to be recognized in ancient environments. In the Palaeozoic, problems of correctly identifying calcareous algae further restrict their use as depth indicators.