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Author information:

1 Alfred Wegener Institute of Polar and Marine Science, Am Alten Hafen 26, 27568 Bremerhaven, Germany 2 Huinay Scientific Field Station, Casilla 462, Puerto Montt, Chile

3 Pontificia Universidad Católica de Valparaíso, Facultad de Recursos Naturales, Escuela de Ciencias del Mar, Avda, Brazil 2950, Valparaíso, Chile

* corresponding author:

christiane.hassenrueck@awi.de

References:

Försterra G, Beuck L, Häussermann V, Freiwald A (2005) Shallow-water Desmophyllum dianthus (Scleractinia) from Chile:

characteristics of the biocoenoses, the bioeroding community, heterotrophic interactions and (paleo)-bathymetric implications, in: Cold-water Corals and Ecosystems. pp. 937–977.

Försterra G, Häussermann V (2008) Unusual symbiotic relationships between microendolithic phototrophic organisms and azooxanthellate cold-water corals from Chilean fjords. Mar Ecol Prog Ser 370, 121–125.

Försterra G, Häussermann V, Mayr C, Jantzen C, Hassenrück C (2012) Low pH and the role of endolithic algae in cold-water corals. International Symposium on Deep-Sea Corals, Amsterdam, Netherlands, April 2-6, 2012.

Roberts J M, Wheeler A J, Freiwald A, Cairns S D (2009) Cold Water Corals. Cambridge University Press. p.234.

Fig. 1: D. dianthus at Fjord Comau infested by O. queckettii (left) and P. terebrans (right);

modified after Försterra & Häussermann (2008).

GROWTH RATES AND SKELETAL DENSITY OF DESMOPHYLLUM

DIANTHUS - EFFECT OF ASSOCIATION WITH ENDOLITHIC ALGAE

Christiane Hassenrück *

1

, Carin Jantzen

1

, Günther Försterra

2,3

and Verena Häussermann

2,3

VII-8

Purpose

The cold-water coral Desmphyllum dianthus is host to two species of endolithic algae: the chlorophyte Ostreobium queckettii and the cyanobacterium Plectonema terebrans (fig. 1). In this association the endoliths occur exclusively in areas of the

skeleton that are covered by coral tissue which has led to the hypothesis that the relationship may be mutually beneficial (Försterra & Häussermann 2008). Such a relationship would be unprecedented since so far no examples of a coral-algal

symbiosis have been documented in cold-water systems. To determine the character of the association between D. dianthus and its endolithic algae growth performance and skeletal density were examined under the assumption that a symbiosis

would positively affect coral calcification.

Fig. 2: Map of the fjord region in southern Chile, D. dianthus sampled at Fjord Comau (red square);

modified after Försterra et al. (2005).

1cm

Fig. 3: Schematic of D. dianthus depicting the plane of the longitudinal sections to measure the linear

extension of septa; modified after Roberts et al. (2009).

Methods

- Sampling site: Fjord Comau, southern Chile (fig. 2)

- D. dianthus stained four times with calcein between January 2006 and 2007 - Coral skeletons sectioned longitudinally (fig. 3) to measure linear apical

extension of septa between individual tips of fluorescent growth bands (fig. 4) - Growth rates tested for an effect of endolithic infestation and seasonality

- Skeletal density determined via x-ray computed tomography (CT)

- Mean density of the apical part of the coral skeleton that had been covered by tissue compared between infested and non-infested individuals

Fig. 4: Longitudinal section of a septum of D. dianthus displaying four distinct growth bands.

Results

Growth rates:

- Median rowth rates of non-infested individuals approx. twice as high as those of infested specimens (t-test on log-transformed data, p<0.05; fig. 5 left)

- Additional to the effect of endolithic infestation: pronounced seasonal pattern of septal growth rates (RM-MANOVA on log-transformed data, p<0.001)

- Contrary to what was expected minimum growth rates coinciding with peak temperatures in summer (Jan ´06 - Apr ´06)

Skeletal density:

- Mean skeletal density of infested individuals approx. 6% lower than that of non-infested polyps (t-test, p=0.146; fig. 6 left)

- Algal infestation affecting skeletal morphology: infested individuals displaying thicker septa, in some cases tumor-like protrusions of septa (fig. 6 right)

Fig. 5: Apical septal growth of non-infested and infested D. dianthus at Fjord Comau averaged over the whole sampling period (Jan ´06 - 2007; left) and among seasons (right), boxplot depicting median, interquartile

range and non-outlier minimum and maximum, empty circles: mild outliers, asterisks: extreme outliers.

Fig. 6 right: Skeletal density of non-infested and infested D. dianthus at Fjord Comau, boxplot set-up similar to fig. 5; left: CT-scan of D. dianthus, upper right hand corner: three-dimensional rendering of apical part of the same infested specimen, thicker skeletal structures compared to non-infested polyps indicated by arrows.

Conclusion

Unlike hypothesized the association between D. dianthus and its endolithic algae has the character of a parasitic relationship. Algal infestation seems to result in significantly reduced growth rates and possibly decreases skeletal density. It may further cause skeletal deformations as a response to the presence of parasites.

The seasonal pattern of apical growth rates of D. dianthus is preserved in infested individuals and may consitute a trade-off between growth and reproduction which is suspected to take place in summer. Although this study appears to conclusively indicate a negative effect of endolithic infestation, controversial results have been obtained by ongoing experiments on the transfer of metabolites between the endoliths and the coral host (Försterra et al. 2012). Further research will be necessary to confirm the status of the relationship between D. dianthus and its endolithic algae.

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