The ingredients for recognizing a bafflestone are the presence of a large number of in-situ stalk-shaped fossils, and a good imagination on the part of the geologist.

Attend a news conference, and prepare a wrap or package.

He is quite disorganized and has difficulty planning his day or remembering when his homework is due.

On the other hand, species lacking zooxanthellae preferentially form solitary coralla or poorly integrated colonies (i.e. with little or no connecting tissue) and have larger corallites; e.g., phaceloid growth forms.