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© Biospeologica Bibliographia - Publications 2010-2

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<strong>©</strong> <strong>Biospeologica</strong> <strong>Bibliographia</strong><br />

<strong>Publications</strong> <strong>2010</strong>-1<br />

Page 50 sur 116<br />

embryos, which increases mouth and taste bud development at the<br />

expense of eyes via pleiotropic Shh signaling. Cavefish lack melanin<br />

synthesis in regressed pigment cells due to loss-of-function mutations in<br />

oca2, which normally regulates the supply of L-DOPA precursor during<br />

melanin synthesis. The block in cavefish pigmentation occurs at a<br />

metabolic branch point in which L-tyrosine is normally converted either<br />

(1) to L-DOPA, DOPAquinone, and melanin by tyrosinase or (2) to L-<br />

DOPA, dopamine, and related catecholamines by tyrosine hydroxylase<br />

and other enzymes. A similar block in the initial step of melanin synthesis<br />

has evolved independently in the cave plant hopper Oliarus polyphemus<br />

and other diverse cave animals. In Astyanax cavefish, the benefit of lost<br />

melanin pigment appears to be the production of excess L-DOPA and its<br />

derivative dopamine by the second alternative pathway, which promotes<br />

constructive development of dopaminergic neurons and enhances the<br />

magnitude of adaptive feeding behavior. We conclude that the evolution<br />

of beneficial constructive traits could have driven regressive traits via<br />

developmental tradeoffs encoded in pleiotropic genes, which adapt cave<br />

animals to life in darkness. http://www.icsb<strong>2010</strong>.net/<br />

JEFFERY (W. R.) & STRICKLER (A. G.), <strong>2010</strong>. Chapter<br />

6. Development as an Evolutionary Process in Astyanax<br />

Cavefishes:141-182. DOI:<br />

http://dx.doi.org/10.1201/EBK1578086702-c6. In:<br />

TRAJANO (E.), BICHUETTE (M. E.) & KAPOOR (B.<br />

G.), Biology of Subterranean Fishes. Edited by TRAJANO<br />

(E.), BICHUETTE (M. E.) & KAPOOR (B. G.). ISBN:<br />

978-1-57808-670-2. eBook ISBN: 978-1-4398-4048-1.<br />

Science Publishers <strong>2010</strong>. 460 p.<br />

JIANG (T.), LIU (R.), METZNER (W.), YOU (Y.), LI (S.),<br />

LIU (S.) & FENG (J.), <strong>2010</strong>. Geographical and individual<br />

variation in echolocation calls of the intermediate leafnosed<br />

bat, Hipposideros larvatus. Ethology 116(8,<br />

August):691-703. DOI: http://dx.doi.org/10.1111/j.1439-<br />

0310.<strong>2010</strong>.01785.x. ABS: The cause and significance of variation in<br />

echolocation call frequency within hipposiderid bats is not well<br />

understood despite an increasing number of allopatric and sympatric<br />

examples being documented. We examined variation patterns in the<br />

resting frequency (RF) of echolocation calls emitted by the intermediate<br />

leaf-nosed bat, Hipposideros larvatus, on a broad geographical scale.<br />

Data mining technology and Kruskal-Wallis test both showed substantial<br />

variation with a longitudinal pattern in RF in H. larvatus among colonies,<br />

and this variation was associated with geographical distance and not body<br />

size. In addition, we found that a high degree of variability between<br />

individuals was hidden under the geographical variation. The results<br />

support an effect of random cultural drift, and challenge the prey<br />

detection hypothesis. Moreover, an acoustic difference among local<br />

island colonies may be indicative of a vocal dialect. We found that each<br />

colony of H. larvatus seems to maintain a "private bandwidth", which<br />

could be used for colony identity and individual communication thus<br />

helping individuals and colonies to get a number of fitness benefits.<br />

JOCHUM (A.), WEIGAND (A. M.), SLAPNIK (R.) &<br />

KLUSSMANN-KOLB (A.), <strong>2010</strong>. Zospeum: Luminaries<br />

of the Dark - Barcoding highlights an old taxonomic<br />

conundrum besetting microsnails (Pulmonata, Ellobioidea,<br />

Carychiidae). Abstract. The Malacological Society of<br />

London Molluscan Forum, Nov. 30, <strong>2010</strong>, NHM London,<br />

UK.<br />

JOHNSON (J. B.), FORD (W. M.), RODRIGUE (J. L.),<br />

EDWARDS (J. W.) & JOHNSON (C. M.), <strong>2010</strong>. Roost<br />

selection by male Indiana myotis following forest fires in<br />

Central Appalachian Hardwoods Forests. Journal of Fish<br />

and Wildlife Management 1(2):111-121; e1944-687X.<br />

DOI: http://dx.doi.org/10.3996/04<strong>2010</strong>-JFWM-007.<br />

JONES (B.), <strong>2010</strong>. Microbes in caves: agents of calcite<br />

corrosion and precipitation:7-30. DOI:<br />

http://dx.doi.org/10.1144/SP336.2. In: PEDLEY (H. M.) &<br />

ROGERSON (M.), Tufas and Speleothems: Unravelling<br />

the Microbial and Physical Controls, Edited by: PEDLEY<br />

(H. M.) & ROGERSON (M.), University of Hull, UK.<br />

Geological Society, London, Special <strong>Publications</strong>, 336.<br />

Bernard LEBRETON & Jean-Pierre BESSON<br />

Créé le : 01.01.<strong>2010</strong><br />

Modifié le : 30.06.<strong>2010</strong><br />

ABS: Diverse biogenic and abiogenic processes produce calcite<br />

speleothems. From a biogenic perspective, cave microbes mediate a wide<br />

range of destructive and constructive processes that collectively influence<br />

the growth of calcite speleothems and their internal fabrics. Destructive<br />

processes include substrate breakdown by dissolution, boring and residue<br />

micrite production, whereas constructive processes include microbe<br />

calcification, trapping and binding of detrital particles to substrates, and<br />

microbial induced calcite precipitation. Biogenesis can be established<br />

from: (1) the presence of mineralized microbes; (2) fabrics, such as<br />

stromatolite-like structures, that can be attributed to microbial activity;<br />

and/or (3) geochemical proxies (carbon and oxygen isotopes, lipid<br />

biomarkers) considered indicative of microbe activity. Such criteria have,<br />

for example, been used to demonstrate microbial involvement in the<br />

formation of pool fingers, stalactites/stalagmites, cave pisoliths and<br />

moonmilk. Nevertheless, absolute proof of microbial biogenesis in<br />

calcitic speleothems is commonly difficult because taphonomic processes<br />

and/or diagenetic processes commonly mask evidence of microbial<br />

activity. The assumption that calcitic speleothems are abiogenic, which<br />

has been tacitly assumed in many studies, is dangerous as there is clear<br />

evidence that microbes thrive in most caves and can directly and<br />

indirectly influence calcite precipitation in many different ways.<br />

JONES (D. S.), TOBLER (D.), SCHAPERDOTH (I.),<br />

MAINIERO (M.) & MACALADY (J. L.), <strong>2010</strong>.<br />

Community structure of subsurface biofilms from the<br />

thermal sulfidic caves of Acquasanta Terme, Italy. Applied<br />

and Environmental Microbiology 76(17, September):5902-<br />

5910. DOI: http://dx.doi.org/10.1128/AEM.00647-10.<br />

JUAN (C.) & EMERSON (B. C.), <strong>2010</strong>. Evolution<br />

underground: shedding light on the diversification of<br />

subterranean insects. Journal of Biology 9(3):17, 5 p. DOI:<br />

http://dx.doi.org/10.1186/jbiol227. ABS: A recent study in BMC<br />

Evolutionary Biology has reconstructed the molecular phylogeny of a<br />

large Mediterranean cave-dwelling beetle clade, revealing an ancient<br />

origin and strong geographic structuring. It seems likely that<br />

diversification of this clade in the Oligocene was seeded by an ancestor<br />

already adapted to subterranean life. See research article<br />

http://www.biomedcentral.com/1471-2148/10/29 webcite.<br />

JUAN (C.), GUZIK (M. T.), JAUME (D.) & COOPER (S.<br />

J. B.), <strong>2010</strong>. Evolution in caves: Darwin's "wrecks of<br />

ancient life" in the molecular era. Molecular Ecology<br />

19(18, September):3865-3880. DOI:<br />

http://dx.doi.org/10.1111/j.1365-294X.<strong>2010</strong>.04759.x. ABS:<br />

Cave animals have historically attracted the attention of evolutionary<br />

biologists because of their bizarre "regressive" characters and convergent<br />

evolution. However, understanding of their biogeographic and<br />

evolutionary history, including mechanisms of speciation, has remained<br />

elusive. In the last decade, molecular data have been obtained for<br />

subterranean taxa and their surface relatives, which have allowed some of<br />

the classical debates on the evolution of cave fauna to be revisited. Here,<br />

we review some of the major studies, focusing on the contribution of<br />

phylogeography in the following areas: biogeographic history and the<br />

relative roles of dispersal and vicariance, colonization history, cryptic<br />

species diversity and modes of speciation of cave animals. We further<br />

consider the limitations of current research and prospects for the future.<br />

Phylogeographic studies have confirmed that cave species are often<br />

cryptic, with highly restricted distributions, but have also shown that their<br />

divergence and potential speciation may occur despite the presence of<br />

gene flow from surface populations. Significantly, phylogeographic<br />

studies have provided evidence for speciation and adaptive evolution<br />

within the confines of cave environments, questioning the assumption<br />

that cave species evolved directly from surface ancestors. Recent<br />

technical developments involving "next generation" DNA sequencing and<br />

theoretical developments in coalescent and population modelling are<br />

likely to revolutionize the field further, particularly in the study of<br />

speciation and the genetic basis of adaptation and convergent evolution<br />

within subterranean habitats. In summary, phylogeographic studies have<br />

provided an unprecedented insight into the evolution of these unique<br />

fauna, and the future of the field should be inspiring and data rich. KW:<br />

Cave animals, cryptic species, phylogeography, speciation, subterranean,<br />

vicariance and dispersal.<br />

JUBERTHIE (C.), <strong>2010</strong>. Jacques Pierre DURAND, 12 Juillet<br />

1936 - 13 Avril 2007. SIBIOS-ISSB Newsletter 7(2006-<br />

<strong>2010</strong>):26-34.

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