scholarly journals Harpacticoida Copepod Associated to Macroalgae Himantothallus Grandifolius (Ochrophyta, Desmarestiaceae) from Admiralty Bay (King George Island, South Shetlands Islands, Maritime Antarctica)

2013 ◽  
pp. 155-159
Author(s):  
Rafael Tostes Salazar ◽  
Geyze Magalhães de Faria ◽  
Tais Maria de Souza Campos ◽  
Adriana Galindo Dalto
2009 ◽  
Vol 44 (8) ◽  
pp. 891-895 ◽  
Author(s):  
Grzegorz Gryziak

This work aimed to investigate the ratio of colonization by terrestrial mites on ice-free areas created by the ongoing climate-induced melting of Antarctic glaciers. Glacier retreat opens new ice-free areas for the colonization by vegetation and animals. The study was undertaken on the Antarctic Specially Protected Area no. 128 (West Coast of the Admiralty Bay, King George Island, South Shetlands Islands). Transects marked between the Ecology, Baranowski and Windy Glaciers, and a sea shore were used to collect soil samples. Oribatid mites were found only on near-shore areas, on patches of vegetation of more than 30 years of age. The colonization by mite communities is strongly determined by the presence of plants.


2011 ◽  
Vol 32 (4) ◽  
pp. 321-340 ◽  
Author(s):  
Karol Zemko ◽  
Saskia Brix

New species of desmosomatid isopods from Admiralty Bay, King George IslandTwo new species of desmosomatid isopods,Eugerdella margaretaesp. n. andEugerdella celatasp. n. are described from Admiralty Bay, King George Island, South Shetlands. Information is added to the original description ofEugerdella falklandica(Nordenstam, 1933) based on re-examination of the holotype. Both new species are similar toE. falklandica, for example by the body shape, the shape of pleotelson and presence of rows of four horn-like spines on the head. They are distinguished fromE. falklandicaby the number of setae on pereopod articles.Eugerdella celatasp. n. is distinguished by the presence of ventral spines on pereonites 1-4.


PeerJ ◽  
2018 ◽  
Vol 6 ◽  
pp. e5408 ◽  
Author(s):  
Marta Potocka ◽  
Ewa Krzemińska

Antarctica, with its severe conditions, is poor in terrestrial fauna species. However, an increase in human presence together with climate change may cause an influx of non-native species. Here we report a significant increase in colonized area of one of the few known invasive species to date in Antarctica. Non-native flies of Trichocera maculipennis have been recently observed in the Admiralty Bay area on King George Island, South Shetlands Islands, West Antarctica, 10 years after its first record in Maritime Antarctica (Maxwell Bay, King George Island). Its rapid spread across the island, despite geographic barriers such as glaciers, indicates successful adaptation to local environmental conditions and suggests this species is invasive. The mode of life of T. maculipennis, observed in natural and anthropogenous habitat and in laboratory conditions, is reported. The following adaptations enabled its invasion and existence within the sewage system in Antarctic scientific stations: the ability to survive in complete darkness, male ability to mate on the substrate surface without prior swarming in flight, and adaptation of terrestrial larvae to survive in semi-liquid food. Possible routes of introduction to Antarctica and between two bays on King George Island are discussed, as well as further research leading to the containment and eradication of this species.


2010 ◽  
Vol 23 (1) ◽  
pp. 27-33 ◽  
Author(s):  
Eduardo de Sá Mendonça ◽  
Newton La Scala ◽  
Alan Rodrigo Panosso ◽  
Felipe N.B. Simas ◽  
Carlos E.G.R. Schaefer

AbstractSoil CO2 emission is an important part of the terrestrial carbon cycling and is influenced by several factors, such as type and distribution of vegetation. In this work we evaluated the spatial variability of soil CO2 emission in terrestrial ecosystems of maritime Antarctica, under two contrasting vegetation covers: 1) grass areas of Deschampsia antarctica Desv., and 2) moss carpets of Sanionia uncinata (Hedw.) Loeske. Highest mean emission was obtained for the Deschampsia (4.13 μmol m-2 s-1) developed on organic-rich soil with a strong penguin influence. The overall results indicate that soil temperature is not directly related to the spatial pattern of soil CO2 emission at the sites studied. Emission adjusted models were Gaussian and exponential with ranges varying from 1.3 to 2.8 m, depending on the studied site and vegetation cover.


2007 ◽  
Vol 107 (4) ◽  
pp. 464-474 ◽  
Author(s):  
Isaac R. Santos ◽  
Déborah I.T. Fávaro ◽  
Carlos E.G.R. Schaefer ◽  
Emmanoel V. Silva-Filho

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