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Marine Botany
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Monterey
Bay Flora
Methods PHYCOLOGICAL SOCIETY OF AMERICA |
Prionitis lanceolataHome Taxonomy Morphology Life History Ecology Gallery Glossary Galls Prionitis covered with tons of galls (circled in blue). See below for better close-ups of the galls. Galls have been observed on Prionitis since Prionitis itself was first described. They were originally thought to be a parasitic red alga called Lobocolax deformans. They are most commonly found on individuals in the low intertidal and subtidal in areas subject to high wave action. Gall formation has been reported on Prionitis lanceolata from Washington, Oregon, California, Peru, and Chile. The galls are light pink to red tumorous domes that protrude from the thallus* of Prionitis and can be 1-15 mm in size. They exhibit uncontrolled growth, are undifferentiated, and the cells are very irregular in shape and structure. Close-up
of a magnificent gall More
recently, it has been determined that the galls are produced when
a specific bacterium comes in direct contact with the medulla* of Prionitis.
This can only occur when Prionitis has been previously wounded.
The bacterium can then enter through the wound to induce gall formation.
The bacterium has not yet been isolated, but there is evidence that
it is a close relative to Roseobacter denitrificans, a parasite
that has been isolated from Ulva in Japan. These bacteria
can be found between the gall cells but not in the normal host tissue.
There is evidence of coevolution between Prionitis and the
bacteria, since a specific bacterium induces galls in Prionitis
lanceolata, while another specific bacterium induces galls in Prionitis
lyallii, etc. Cross section of the outgrowth. The gall is clearly derived from medullary tissue, which then disrupts the cortex to emerge. Created by Alice Chiu, 2003. Images may be used with permission. |
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