Mostrando entradas con la etiqueta Ophiosteira. Mostrar todas las entradas
Mostrando entradas con la etiqueta Ophiosteira. Mostrar todas las entradas

Gigantism and dwarfism


Gigantism is well known among Antarctic benthic organisms, although the fact is that size abnormalities occur in both directions (gigantism and dwarfism). Is it possible that it would be a case of evolution with a disruptive selection in which the organisms with extreme phenotypes would be the dominant forms?  That means, being small size organisms (ophiuroids with disc less than 5mm) and large size ones (ophiuroids with disk of about 30mm) more abundant in species compared to the middle size organisms (ophiuroids with disk of approximately 10 mm).



The origin of dwarfism seems to be found in the difficulty to precipitate calcium carbonate at low temperatures, which is supposed to be a limiting factor for organisms with calcareous skeletons, such as calcareous foraminifera, prosobranch gastropods, bivalves and brachiopods, among which we can find Antarctic species of very small size. Antarctic echinoderms with a skeleton composed of calcareous dermal ossicles are “doomed” to higher energy consumption in order to incorporate calcium carbonate, compared to echinoderms from other geographical areas, for this reason, it seems logical to consider this enviroment to be a hostile one for this zoological group development, although it does not look to be like that, as  the echinoderms are among the benthic groups with most diversity and biomass in the Antarctic benthos.
Whatever the case and considering dwarf ophiuroid species those that do not reach 5 mm disk diameter , we have: Ophiacantha paramedea, Ophiomitrella ingrata, Amphiophiura antarctica, Ophiocten banzarei, Ophiocten bisquamatum, Ophiomastus conveniens, Ophiomastus ludwigi, Ophiomastus perforatus, Ophiomastus primula, Ophiomastus trispinosus, Ophiosteira bullivanti, Ophiopyrgus australis, Amphiura lymani,  Amphiura algida, Amphiura microplax, Amphiura monorima and Ophiozonella antarctica.


Antarctic animals with siliceous skeletons or those with no mineralized skeleton, can multiply by up to ten the size of the individuals of the species compared to ones of the same groups in other geographical areas, as it happens to nemerteans, pycnogonids and giant isopods, like if meeting the Bergmann’s rule. The waters with low temperatures and seasonal food shortages (in winter) reduce basal metabolism which may cause a delay in sexual maturity and increased longevity, the two factors that, along with  an environment with little amount of predators can favor the development of a giant size.
Among the ophiuroids, even despite its calcareous skeleton, appear giant Antarctic species, considering giant the species with disk diameter over 30 mm, we have: Gorgonocephalus chilensis  (though the gorgonocephalids in general have large size) Astrotoma agassizii, Ophiosparte gigas, Ophionotus victoriae, Ophionotus hexactis, Ophiura flexibilis, Ophiura lenticularis, Ophiocamax gigas and Ophiocamax drygalskii.

Taking the data of 117 species of ophiuroids present in Antarctic waters (I’ve excluded those with high distribution outside Antarctic waters) and represented according to disk sizes in ranges, we obtain the following graphic:


It shows a classic Gaussian bell curve, which clearly indicates an evolutionary “stabilizing type” tendency, i.e. where corporal phenotypes of middle size have been selected predominantly
When compared with species from other latitudes as in the case of brittle stars found in British waters (excluding cosmopolitan species), we have the following graphic as a result:


Where we can see presented proportionally even more anomalous cases respecting size.
Therefore it doesn’t seem to be that the dwarfism or gigantism have been selective factors at group level in the Antarctic ophiuroids, but it is more about cases that have to be treated in a particular way.

References
ARNAUD, P.M. 1974. Contribution a la bionomie marine benthique des regions antarctiques et subantartiques. Téthys, 6, 467–653.

SOUTHWARD, E.C. & CAMPBELL, A.C. 2006. Echinoderms. Synopses of the British Fauna. Edited by Crothers, J.H. & Hayward, P.J. The Linnean Society of London and Estuarine and Coastal Sciences Association.

TORTONESE, E. 1965. Echinodermata. Fauna D’Italia. Edizioni Calderini, Bologna.

November 2010

Soy Rafael Martín

Profesor de Biología y Geología en el I.E.S. Santa Bárbara de Málaga. Licenciado en Ciencias Biológicas con especialidad en Zoología y Master en Investigación Científica. 
Estudio organismos marinos de bentos; con especialización en la taxonomía y biogeografía de ofiuroideos (equinodermos) antárticos.

Con un estereomicroscopio (Zeiss Discovery V8) en el Natural History Museum de Londres; viendo especímenes de la expedición Challenger (1872-1876) . 


Así es como llegan los especímenes de las expediciones, conservados en formaldehído o etanol, a la espera de una ardua labor de identificación.

BAS (British Antarctic Survey -Cambridge-).

He realizado estancias de investigación en la British Antarctic Survey (Cambridge; Inglaterra), para el estudio de diversas colecciones de ofiuroideos pertenecientes a expediciones británicas y alemanas al Océano Sur alrededor Antártida.

En el laboratorio de BAS con Chester Sand, ecólogo molecular y Huw Griffths, biogeógrafo marino.

En el laboratorio de BAS con los botes de muestras de ofiuroideos de una expedición británica en aguas del Arco de Scotia en la Antártida; el estereomicroscopio es un Zeiss Stemi SV 6.


En el laboratorio de BAS con estereomicroscopio Leica M65

Ophiosteira bullivanti, fotografía tomada con cámara CCD en un estereomicroscopio Leica M65.


Microscopio electrónico (Quanta 3D FEG/FEI SEM) en la Universidad de Extremadura.

Fotografías SEM (microscopía electrónica de barrido) de Ophiacanta wolftarntzi. Una nueva especie descrita, por el que esto escribe, colectada por el buque de investigación alemán Polarstern en aguas antárticas.

Ofiuroideos antárticos vivos. Estos, conservando su color original, fueron fotografiados momentos después de ser recogidos con una draga Agassiz.

Publicaciones como primer autor:

Brittle stars from Southern Ocean (Echinodermata: Ophiuroidea)

screen-capture

A new brooding species of brittle star (Echinodermata: Ophiuroidea) from Antarctic waters

Publicaciones como coautor:

The macro- and megabenthic fauna on the continental shelf of the eastern Amundsen Sea, Antarctica

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Observations of the ophiuroids from the West Antarctic sector of the Southern Ocean

Against the flow: evidence of multiple recent invasions of warmer continental shelf waters by a Southern Ocean brittle star
Frontiers

Para saber más sobre los ofiuroideos antárticos puedes hacer click sobre la siguiente imagen:



Roofs and eyeglasses in Antarctic ophiuroids


In 1961 Fell, in his monograph on the Ross Sea Ophiuroidea, drew attention to the development of skeletal excrecence in Antarctic ophiuroids from Euvondrea and Ophiosteira genera. Fell found no explaination for these outgrowths.


These expansions, especially in the dorsal arm plates, can also be seen in other Antarctic species such as Ophiura (Ophiuroglypha) carinifera, Anophiura banzarei, Ophiomages cristatus, Ophiomastus bispinosus and some species of Ophioplinthus genus.


Ignoring the mere evolutionary whim, there could be various interpretations. For example, passive defense: the protrusive elements could dissuade the predators which would prefer something easier to chew and swallow. Or, acting as peaked roofs somewhere in Siberia or Pirinei Mountains –  little flat surface on aboral part protects them from heavy “snowfalls” and, so, doesn’t let them be buried in funds with a high degree of sedimentation. Or, the explanation could be the possible presence of amplifier lenses for photoreception (see symmetrical structures as honeycomb cells of Ophiosteira).


At any rate, nature manifests its spectacularity through the tiniest details of organisms which did not evolve to amaze us, nonetheless, we can’t help being marvelled at them.



November 2011