Symbiont transmission in the hydrothermal vent tubeworms
Andrea Nussbaumer &
Monika Bright
Department of Marine Biology,
Institute of Ecology and Conservation Biology, University of Vienna, Austria
The uptake of symbionts in hydrothermal vent tubeworms
(Vestimentifera, Siboglinidae) is facilitated by massive infection of the skin
and simultaneous apoptosis. This mechanism, well known from pathogenic
infection, leads here to the development of a new mesodermal organ, the
trophosome, in the interior of the worm’s trunk and thus to the establishment
of a nutritional association beneficial for both partners. We investigated
settled tubeworm larvae and early juveniles from 200 to 500 µm, collected
during three cruises to the East Pacific Rise, 9°50N, in 1998, 1999, 2001. Serial
transmission electron microscopical sections showed infection of the epidermis,
somatic muscles and mesenchym through symbiont like bacteria. Apoptosis was apparent
in these infected as well as in adjacent cells by cell shrinkage, pycnotic
nuclei with dense chromatin masses accumulating peripherally and dilated
mitochondria. Fluorescence in situ Hybridization using a 16S rRNA
symbiont-specific probe identified these bacteria as symbionts. Additional
analyses with various group-specific eubacteria and archaea probes showed that
neither the infected skin nor the developing trophosome harbored other than
the symbiotic phylotype.
The current hypothesis proposes the establishment of the
symbiosis being by uptake of symbionts through the digestive system of the
early juvenile followed by proliferation of the endodermal midgut cells,
transformation into bacteriocytes and development of the trophosome from
endodermal tissue. Our
findings point to a different pathway: bacteria infect the skin and trigger
apoptosis, which probably facilitates migration into deeper layers until the
visceral mesoderm is reached. The symbionts are then enclosed in vacuoles and
the mesoderm proliferates to form the trophosome.
Infection
and apoptosis facilitate transmission of symbionts and establishment of
endosymbiosis in hydrothermal vent tubeworms
Bright M1.,
Fisher C. R.2, Nussbaumer A. 1
1Institute of Ecology and Conservation Biology,
University of Vienna, Althanstr. 14, A-1090 Vienna, Austria
2The Pennysylvania
State University, 208 Mueller Lab, University Park, PA 16802-5301, USA
The
current hypothesis proposes that the transmission and establishment of the symbiosis between hydrothermal vent
tubeworms (Vestimentifera, Siboglinidae) and thiotrophic endosymbionts is by
uptake of symbionts through the digestive system in early juveniles into
endodermal mitgut cells, followed by proliferations and transformation of
midgut cells into bacteriocytes, and development of the trophosome. Our findings point to a different pathway:
bacteria infect the skin and trigger apoptosis, which probably facilitates
migration into deeper layers until the visceral mesoderm is reached. The
symbionts are then enclosed in vacuoles and the mesoderm proliferates to form
the trophosome. We investigated settled tubeworm larvae and early juveniles
(200 - 500 µm in length), collected during three cruises to the East Pacific
Rise, 9°50N, in 1998, 1999, and 2001. Serial transmission electron
microscopical sections showed that the epidermis, somatic muscles, and
mesenchym are infected with symbiont-like bacteria in early juveniles.
Apoptosis was apparent in these tissues by cell shrinkage, pycnotic nuclei with
dense chromatin masses accumulating peripherally and dilated mitochondria. Fluorescence
in situ Hybridization was applied on a different set of animals using a 16S
rRNA symbiont-specific probe. The bacteria in the skin were identified as
symbionts. Additional analyses with various group-specific eubacteria and
archaea probes showed that neither the infected skin nor the developing
trophosome harbored other than the symbiotic phylotype.
Discovery
of a new symbiosis from antarctic, shallow-water hydrothermal vents
Bright, M.1, C. Arndt2,3,
H. Keckeis1 and H. Felbeck3
1Institute of Ecology and Conservation Biology,
University of Vienna, Althanstr. 14, A-1090 Vienna, Austria
2Institute for Microbiology, Ernst-Moritz-Arndt
University, Friedrich-Ludwig-Jahn Strasse 15, D-17489 Greifswald, Germany
3Scripps Institution of Oceanography, University of
California San Diego, La Jolla, CA 92093-0202, USA
A prominent not further identified species of
Monocelidae (Plathelminthes, Proseriata) was identified in the vicinity of
fumarole activity at Fumarole Bay (Deception Island, Antarctica). Apparently
symbiotic, monotypic curved rods colonized the surface of the animals.
Investigating the distribution of this animal and the metazoan meiobenthos in
and in the vicinity of this area we infer that this species constitutes the
most abundant species and the bulk of the biomass at these shallow water
hydrothermal vent sediments. In contrast to the other metazoan meiofauna, the
distribution of this species is positively correlated with the water
temperature and gas emissions indicating a preference for the areas around
fumaroles. The range of temperature tolerated by this symbiosis was determined
in in vivo experiments to be at least
30°- 40°C.
The results of this study revealed a remarkable
difference between shallow water and deep-sea hydrothermal vent meiobenthic
communities. Generalists capable of tolerating extreme abiotic conditions
appear to dominate shallow water vents, whereas endemism seems to be the rule
in the deep-sea vents. A symbiotic life style apparently has evolved among
meiofaunal representatives of shallow water vents, while it has not been
described for any meiofaunal species from deep-sea vents.
The color of the trophosome: elemental sulfur
distribution in the endosymbionts of Riftia
pachyptila, Jones 1981
(Vestimentifera, Siboglinidae)
Pflugfelder B. 1, Fisher C. R.2,
Bright M1
1Institute of Ecology and Conservation Biology,
University of Vienna, Althanstr. 14, A-1090 Vienna, Austria
2The Pennysylvania
State University, 208 Mueller Lab, University Park, PA 16802-5301, USA
The presence of elemental sulfur stored in
vesicles of thiotrophic free-living or symbiotic bacteria is known to serve as
energy source for sulfide oxidation. Such vesicles do occur in the
chemoautotrophic sulfide-oxidizing symbionts of Riftia pachyptila (Vestimentifera, Siboglinidae), but neither the
content of these vesicles was analyzed, nor their density in the different
morphotypes in different regions of the trophosome from different animals.
However, bulk chemical analyses showed that the specific color of the
trophosome is related to the amount of elemental sulfur (Fisher xy?). The
objectives of this study were to detect elemental sulfur in the vesicles of the
symbionts by Electron Energy Loss Spectrography (EELS) and subsequently to
investigate the density of sulfur vesicles (SD) by quantitative Transmission
Electron Microscopy (TEM) and stereological techniques using SD values that
express the percentage of the symbiotic cytoplasm area taken up by vesicles in
ultrathin sections for comparisons: 1) three animals each with uniformly
colored trophosomes; two animals with trophosome color changing from anterior
to posterior; 2) three trophosomal regions (anterior, median, and porsterior),
and 3) three trophosomal lobule zones (central rods, median small cocci, peripheral
large cocci).
The SD highly
correlated with the color of the trophosome. This was found in animals with
uniformly colored trophosomes as well as trophosomes that exhibit a gradual
color change from the anterior to the posterior. A relative SD decrease of 40%
was found between animals with light and dark green trophosomes and another 40%
decrease between dark green and black. All animals were collected from a single
site extending a few m2 but the amount of sulfur storage points to a
highly variable supply of sulfide. In this respect, the color of the trophosome
is a useful tool to estimate the chemical condition under which a specific
tubeworm thrives.
In animals with
light green trophosomes, we found a significant decrease in SD from the
peripherally located cocci to the centrally located rods. This gradient,
although it follows the direction of blood flow in the trophosome lobule and
thus theoretically the supply of sulfide for sulfide oxidation and sulfur
storage, cannot be explained as limitations of sulfide in rods. Support comes
from animals with black and dark green trophosomes, in which no SD gradient in
morphotypes was found. This points to a lower but similar supply of sulfide for
all symbionts than in those animals with light green trophosome. Although the
specific underlying mechanisms remain to be clarified, we hypothesize that the
rods and cocci behave physiologically different when exposed to high sulfide
concentrations but perform similar under lower sulfide concentrations.