Abstract:
Flakes detached from rocks of a volcano rivulet at
‘National Park Rincón de la Vieja Volcano’, Guanacaste,
Costa Rica, revealed a green layer 2–3 mm deep into
the rock matrix. Analysis by scanning electron microscopy
showed a complex assemblage of microorganisms,
beginning with a thin layer of Cyanidium and followed
by diatoms of the genus Pinnularia and curved and
straight bacteria. To our knowledge, this is the first
description of an endolithic microbial consortium dominated
by diatoms, and also the first report of endolithobionts
from volcanic rocks in a tropical area.