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Journal articles on the topic 'Livingston Island'

Author: Grafiati

Published: 4 June 2021

Last updated: 27 July 2025

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1

García-Álvarez, Oscar, and Victoriano Urgorri. "Solenogastres molluscs from the BENTART Collection (South Shetland Islands, Antarctica), with a description of a new species." Iberus 21(1) (June 30, 2003): 43–56. https://doi.org/10.5281/zenodo.4515825.

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Four specimens from the BENTART Collection are studied (South Shetland Islands and Bransfield Strait, Antarctic). Two specimens were identified as: <em>Rhopalomenia carinata </em>Salvini-Plawen, 1978 collected on a muddy, gravel bottom at a depth of 710 m, off Livingston Island, and <em>Rhopalomenia rhynchopharyngeata </em>Salvini-Plawen, 1978 from a muddy bottom at a depth of 235 m off Livingston Island. One specimen, collected from a fine muddy and sandy bottom at a depth of 80 m off Livingston Island, belongs to the genus <em>Neomenia</em>, presenting features which well distinguish the sam

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Apostolov, Apostol. "Paralaophonte livingstoni n. sp. (Crustacea: Copepoda: Harpacticoida) -- un nouveau representant de l'ile de Livingstone, Antarctique." Historia naturalis bulgarica 16 (September 20, 2004): 59–67. https://doi.org/10.5281/zenodo.4043166.

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One new marine harpacticoid copepod, Paralaophonte livingstoni n.sp., is described. It has been collected only in the coastal zooplankton of the Marine Lion bay and north of the South Bay of the Livingston Island, Antarctic. The new species is characterized by the armament of P2 -- P5 and furca. The affinities and systematic position of the new species are discussed.

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3

Stehberg, Ruben, Michael Pearson, Robert Blanchette, and Joel A. Jurgens. "A further note on a sealer's sledge, discovered on Livingston Island, South Shetland Islands." Polar Record 45, no. 3 (2009): 275. http://dx.doi.org/10.1017/s0032247409008201.

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Pearson, Michael, Ruben Stehberg, Andres Zarankin, Maria Ximena Senatore, and Carolina Gatica. "Sealer's sledge excavated on Livingston Island, South Shetland Islands." Polar Record 44, no. 4 (2008): 362–64. http://dx.doi.org/10.1017/s0032247408007687.

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5

Burfeid-Castellanos, Andrea M., Rafael P. Martín-Martín, Michael Kloster, Carlos Angulo-Preckler, Conxita Avila, and Bánk Beszteri. "Epiphytic diatom community structure and richness is determined by macroalgal host and location in the South Shetland Islands (Antarctica)." PLOS ONE 16, no. 4 (2021): e0250629. http://dx.doi.org/10.1371/journal.pone.0250629.

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The marine waters around the South Shetland Islands are paramount in the primary production of this Antarctic ecosystem. With the increasing effects of climate change and the annual retreat of the ice shelf, the importance of macroalgae and their diatom epiphytes in primary production also increases. The relationships and interactions between these organisms have scarcely been studied in Antarctica, and even less in the volcanic ecosystem of Deception Island, which can be seen as a natural proxy of climate change in Antarctica because of its vulcanism, and the open marine system of Livingston

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Vijver, Bart Van De, and Ralitsa Zidarova. "Five new taxa in the genus Pinnularia sectio Distantes (Bacillariophyta) from Livingston Island (South Shetland Islands)." Phytotaxa 24 (December 31, 2011): 39–50. https://doi.org/10.11646/phytotaxa.24.1.6.

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Vijver, Bart Van De, Zidarova, Ralitsa (2011): Five new taxa in the genus Pinnularia sectio Distantes (Bacillariophyta) from Livingston Island (South Shetland Islands). Phytotaxa 24: 39-50, DOI: 10.11646/phytotaxa.24.1.6

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Sancho, Leopoldo G., Florian Schulz, Burkhard Schroeter, and Ludger Kappen. "Bryophyte and lichen flora of South Bay (Livingston Island: South Shetland Islands, Antarctica)." Nova Hedwigia 68, no. 3-4 (1999): 301–37. http://dx.doi.org/10.1127/nova.hedwigia/68/1999/301.

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8

Kopalova, Katerina, Ryszard Ochyra, Linda Nedbalová, and de Vijver Bart Van. "Moss-inhabiting diatoms from two contrasting Maritime Antarctic islands." Plant Ecology and Evolution 147, no. (1) (2014): 67–84. https://doi.org/10.5091/plecevo.2014.896.

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<b>Background and aims</b> – The Maritime Antarctic vegetation is a poorly developed tundra dominated by lichens and mosses, mostly present in moist environments, providing a favourable habitat for microorganisms. Although, diatoms represent one of the most common algal groups in the Antarctic region, moss-inhabiting diatoms are rarely studied. The moss vegetation on islands in the Maritime Antarctic region forms a favorable habitat for non-marine diatoms. These moss-inhabiting diatom communities are of particular interest as little is known about their species composition, ecological preferen

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Golemansky, Vassil. "SYNTHESIS OF THE BULGARIAN PROTOZOOLOGICAL INVESTIGATIONS OF SOUTH SHETLAND ISLANDS (THE ANTARCTIC)." Ecologica Montenegrina 5 (February 17, 2016): 47–56. http://dx.doi.org/10.37828/em.2016.5.9.

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Within the range of the Bulgarian Antarctic Program (1987-2010) some parasitological investigations on the coccidian parasites of 3 penguin species from South Shetland Islands (Livingston and St George Islands) were conducted, namely: Pygoscelis antarctica, P. papua and P. adeliae. Three coccidian species were found, one of which was described as a new species: Eimeria pygosceli Golemansky, 2003. It was isolated from the fecal samples of all 3 penguin species, living at South Shetland Islands. The other not identified coccidian’s were of the genera Eimeria and Isopspora. (Table 1). The great n

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Golemansky, Vassil. "Coccidian parasites (Apicomplexa) of penguins (Pygoscelis ssp.) from Livingston Island and King George Island, the Antarctic." Polish Polar Research 32, no. 3 (2011): 263–68. http://dx.doi.org/10.2478/v10183-011-0018-4.

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Coccidian parasites (Apicomplexa) of penguins (Pygoscelis ssp.) from Livingston Island and King George Island, the Antarctic The results of investigations on the coccidian parasites of three species of penguins (Pygoscelis antarctica, P. papua and P. adeliae), nesting at Livingston and King George Island (South Shetland Islands, the Antarctic) are presented. Three coccidian parasites: Eimeria pygosceli Golemansky, 2003, Eimeria sp. and Isospora sp. were identified in faecal samples from 360 examined birds. The total prevalence of coccidian parasites was high: about 35% in all of examined pengu

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Schroeter, Burkhard, T. G. Allan Green, Stefan Pannewitz, Mark Schlensog, and Leopoldo G. Sancho. "Fourteen degrees of latitude and a continent apart: comparison of lichen activity over two years at continental and maritime Antarctic sites." Antarctic Science 22, no. 6 (2010): 681–90. http://dx.doi.org/10.1017/s0954102010000647.

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AbstractThere are marked declines in precipitation, mean temperatures and the number of lichen species with increasing latitude in Antarctica. However, it is not known which factors are the predominant controllers of biodiversity changes. Results are presented from over two years of almost continuous monitoring of both microclimate and activity in lichens at Livingston Island, South Shetland Islands, 62°S, and Botany Bay, Ross Sea region, 77°S. Lichen activity was evident over a much longer period at Livingston Island, (3694 versus 897 hours) and could occur in any month whereas it was almost

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Zidarova, Ralitsa, Kateŕina Kopalová, and Bart Van De Vijver. "The genus Pinnularia (Bacillariophyta) excluding the section Distantes on Livingston Island (South Shetland Islands) with the description of twelve new taxa." Phytotaxa 44 (February 6, 2012): 11–37. https://doi.org/10.11646/phytotaxa.44.1.2.

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Zidarova, Ralitsa, Kopalová, Kateŕina, Vijver, Bart Van De (2012): The genus Pinnularia (Bacillariophyta) excluding the section Distantes on Livingston Island (South Shetland Islands) with the description of twelve new taxa. Phytotaxa 44: 11-37, DOI: 10.11646/phytotaxa.44.1.2, URL: https://www.biotaxa.org/Phytotaxa/article/view/phytotaxa.44.1.2

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13

Vlček, Vítězslav, David Juřička, and Jitka Míková. "Heavy metal concentration in selected soils and sediments of Livingston Island, Deception Island, King George Island, James Ross Island (Antarctica)." Czech Polar Reports 7, no. 1 (2017): 18–33. http://dx.doi.org/10.5817/cpr2017-1-3.

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This paper evaluated the heavy metal concentration in fine earth and skeleton fraction of the Antarctic soil and sediments in the Admiralty Bay (King George Island); Livingston Island; Whaler´s Bay (Deception Island); James Ross Island and the Trinity peninsula (Antarctica). Total concentrations of eight elements (arsenic, chromium, copper, nickel, lead, strontium, vanadium, and zinc) were determined in sixteen sediments/soils samples and skeleton fraction. For the analyses, eight samples were taken from James Ross Island, four samples from Deception Island, two samples from Trinity peninsula,

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Bañón, Manuel, Ana Justel, David Velázquez, and Antonio Quesada. "Regional weather survey on Byers Peninsula, Livingston Island, South Shetland Islands, Antarctica." Antarctic Science 25, no. 2 (2013): 146–56. http://dx.doi.org/10.1017/s0954102012001046.

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AbstractIn 2001 the LIMNOPOLAR Project was launched with the aim of addressing the suitability of freshwater ecosystems as useful sentinels of climate change. In this project, an automatic weather station was deployed on Byers Peninsula (Livingston Island, South Shetland Islands) near several freshwater ecosystems under research. Here the multi-year data recorded are presented and compared with meteorological time series from the observatories at the Spanish Juan Carlos I Station, Deception Island and Bellingshausen Station. Lake freezing and thawing periods and snow cover are also investigate

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15

Valladares, Fernando, and Leopoldo G. Sancho. "Lichen Colonization and Recolonization of Two Recently Deglaciated Zones in the Maritime Antarctic." Lichenologist 27, no. 6 (1995): 485–93. http://dx.doi.org/10.1016/s0024-2829(95)80008-5.

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AbstractThe stages of vegetation development close to two glacier fronts on two of the South Shetland Islands (Livingston and Robert) within the Maritime Antarctic were studied with special reference to saxicolous lichens. A lichenometric study of the crustose lichen Caloplaca sublobulata was carried out at both sites. On the moraine of Livingston Island, rock size played an important role in lichen development, explaining most of the differences observed in the diameter of C. sublobulata, the number of species, and the percentage of cover among the rocks studied. On Robert Island, the distanc

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Blanco, Juan José, Juan Ignacio García-Tejedor, Óscar García-Población, et al. "Cosmic ray observations from Livingston Island." Advances in Space Research 69, no. 9 (2022): 3514–24. http://dx.doi.org/10.1016/j.asr.2022.02.046.

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Pavlova, K., D. Grigorova, T. Hristozova, and A. Angelov. "Yeast strains from Livingston Island, Antarctica." Folia Microbiologica 46, no. 5 (2001): 397–401. http://dx.doi.org/10.1007/bf02814428.

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18

Schroeter, Burkhard, T. G. Allan Green, Ana Pintado, Roman Türk, and Leopoldo G. Sancho. "Summer activity patterns for mosses and lichens in Maritime Antarctica." Antarctic Science 29, no. 6 (2017): 517–30. http://dx.doi.org/10.1017/s095410201700027x.

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AbstractWithin Antarctica there are large gradients both in climate and in vegetation which offer opportunities to investigate links between the two. The activity (% total time active) of lichens and bryophytes in hydric and xeric environments was monitored at Livingston Island (62°39'S). This adds a northern site with a maritime, cloudy climate to previous studies in the southern Antarctic Peninsula and the Dry Valleys (78°S). Annual activity increases northwards from less than 1% to nearly 100%. There is a major and consistent difference between hydric sites which, with snow melt, can be 100

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19

Jones, V. J., S. Juggins, and J. C. Ellis-Evans. "The relationship between water chemistry and surface sediment diatom assemblages in maritime Antarctic lakes." Antarctic Science 5, no. 4 (1993): 339–48. http://dx.doi.org/10.1017/s095410209300046x.

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Maritime Antarctic freshwater lakes and their catchments are inherently simple systems in an environment which is characterized by strong seasonality. Such lakes offer excellent opportunities to study the interaction of water chemistry and plant communities. The response of diatom species to environmental gradients was assessed by constructing a diatom and water chemistry dataset from 59 lakes at two locations (Livingston Island, South Shetland Islands and Signy Island, South Orkney Islands). Results indicate that diatom species abundance is predominately related to nutrient and salinity gradi

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Willan, Robert C. R. "Preliminary field observations on peperites and hydrothermal veins and breccias on Livingston Island, South Shetland Islands." Antarctic Science 4, no. 1 (1992): 109–10. http://dx.doi.org/10.1017/s0954102092000166.

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Sulphide-bearing quartz veins were first observed on Hurd Peninsula, Livingston Island, at Henry Bluff in 1958 (Hobbs 1968). Subsequent mapping of the host Miers Bluff Formation (MBF) in western Hurd Peninsula either did not record veining or was ambiguous as to its distribution, scale of development and genesis (for review see Pride et al. 1990).

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21

Osmanoglu, B., M. I. Corcuera, F. J. Navarro, M. Braun, and R. Hock. "Frontal ablation and temporal variations in surface velocity of Livingston Island ice cap, Antarctica." Cryosphere Discussions 7, no. 4 (2013): 4207–40. http://dx.doi.org/10.5194/tcd-7-4207-2013.

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Abstract. Frontal ablation from marine-terminating glaciers and ice caps covering the islands off the western coast of the Antarctic Peninsula is poorly known. Here we estimate the frontal ablation from the ice cap of Livingston Island, the second largest island in the South Shetland Islands archipelago, using glacier surface velocities obtained from intensity offset tracking of PALSAR-1 imagery and glacier ice thickness inferred from principles of glacier dynamics and calibrated against ground-penetrating radar (GPR) measurements of ice thickness. Using 21 SAR images acquired between October

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22

Abad, F. Xavier, Núria Busquets, Azucena Sanchez, Peter G. Ryan, Natàlia Majó, and Jacob Gonzalez-Solís. "Serological and virological surveys of the influenza A viruses in Antarctic and sub-Antarctic penguins." Antarctic Science 25, no. 2 (2013): 339–44. http://dx.doi.org/10.1017/s0954102012001228.

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AbstractTo evaluate the avian influenza virus (AIV) circulation in Antarctic and sub-Antarctic penguins we carried out a serosurvey on six species from Livingston, Marion and Gough islands. Seropositivity against AIV was performed on serum samples using a competitive enzyme-linked immunosorbent assay and haemagglutination and neuraminidase inhibition assays. Some oropharyngeal and cloacal swabs were also assayed to detect influenza virus genomes by real time reverse transcription-polymerase chain reaction. Overall, 12.1% (n= 140) penguins were seropositive to AIV. By species, we detected 5% (n

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23

García-Alvarez, O., V. Urgorri, and L. von Salvini-Plawen. "Two new species of Dorymenia (Mollusca: Solenogastres: Proneomeniidae) from the South Shetland Islands (Antarctica)." Journal of the Marine Biological Association of the United Kingdom 80, no. 5 (2000): 835–42. http://dx.doi.org/10.1017/s0025315400002812.

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This paper describes two new species from the genus Dorymenia (Mollusca: Solenogastres: Proneomeniidae): D. hesperidesi sp. nov. and D. menchuescribanae sp. nov., collected during the Spanish oceanographic expeditions for the study of Antarctic benthos, BENTART'94 and BENTART'95, carried out in the area of the Livingston Island (South Shetland Islands, Antarctica). A comparative study of main specific characteristics of species belonging to the genus Dorymenia found off the South Shetland Islands and in the Bransfield Strait (Antarctica), is also included.

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León, Tomás Munilla. "Ammothea tibialis, a new pycnogonid from Drake Passage, Antarctica." Antarctic Science 14, no. 2 (2002): 171–73. http://dx.doi.org/10.1017/s0954102002000731.

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The most recent reports about the family Ammotheidae of pycnogonids from Southern Ocean waters are those of Munilla (2000, 2001, Scotia Sea), Pushkin (1993, various zones), Bamber (1995, Falkland Islands and South Shetland Islands) and Child (1994, various zones) who also provide historical background. Some species from Livingston Island and surrounding waters (South Shetland Islands, Drake Passage, Bransfield Strait) have been documented previously, mainly by Gordon (1932), Fry & Hedgpeth (1969), Pushkin (1993) and the papers of Child and Bamber mentioned above. Keys to this genus are giv

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Griffiths, Huw J., Katrin Linse, and David K. A. Barnes. "Distribution of macrobenthic taxa across the Scotia Arc, Southern Ocean." Antarctic Science 20, no. 3 (2008): 213–26. http://dx.doi.org/10.1017/s0954102008001168.

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AbstractAn extremely dynamic chain of archipelagos links South America and the Antarctic Peninsula. It includes islands, which are large and small, old and young, near continental margins and isolated, and well sampled and poorly known. The current study sampled the macrobenthos of all the major archipelagos of this arc at shelf and slope depths using an Agassiz trawl. At least four samples (200 m, 500 m, 1000 m and 1500 m) were taken down-slope at Falkland Trough, Shag Rocks, South Georgia, South Thule, Powell Basin, Elephant Island, and Livingston Island sites and one sample was collected in

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León, Tomás Munilla. "A new species of Ammothea and other pycnogonids from around Livingston Island, South Shetland Islands, Antarctica." Antarctic Science 12, no. 1 (2000): 47–51. http://dx.doi.org/10.1017/s0954102000000079.

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Specimens of 22 species of pycnogonids belonging to twelve genera and seven families were collected during a cruise near Livingston Island, South Shetland Islands. Twenty two of the 94 stations yielded pycnogonids: the new species Ammothea hesperidensis is described fully, illustrated, and compared with similar species. The family Nymphonidae provided both the greatest diversity of species (seven) and number of specimens (35). The most abundant species were Achelia hoekii and Nymphon australe.

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Sancho, L. G., L. Kappen, and B. Schroeter. "The lichen genus Umbilicaria on Livingston Island, South Shetland Islands, Antarctica." Antarctic Science 4, no. 2 (1992): 189–96. http://dx.doi.org/10.1017/s0954102092000294.

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Five species of Umbilicaria are described, three of which, U. africana, U. krascheninnikovii and U. nylanderiana, have not been previously recorded from Antarctica. Distributional patterns and morphological characteristics of these species are discussed.

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Zidarova, Ralitsa, de Vijver Bart Van, Antonio Quesada, and Haan Myriam De. "Revision of the genus Hantzschia (Bacillariophyceae) on Livingston Island (South Shetland Islands, Southern Atlantic Ocean)." Plant Ecology and Evolution 143, no. (3) (2010): 318–33. https://doi.org/10.5091/plecevo.2010.402.

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<b>Background and aims</b> – The non-marine diatom flora of Livingston Island (South Shetland Islands, Maritime Antarctic Region) is currently under revision. One of the genera that still needed a revision is the genus <i>Hantzschia</i>, quite common in terrestrial habitats of the Antarctic Region. <b>Methods</b> – Using both Light Microscopical and Scanning Electron Microscopical techniques, the morphology of all <i>Hantzschia</i> taxa, present in the samples from Livingston Island, has been analysed. Each taxon is compared with all other possible similar <i>Hantzschia</i> taxa, known worldwi

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Grad, M., A. Guterch, and P. Środa. "Upper crustal structure of Deception Island area, Bransfield Strait, West Antarctica." Antarctic Science 4, no. 4 (1992): 469–76. http://dx.doi.org/10.1017/s0954102092000683.

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This paper describes the results of seismic refraction investigations of the upper crustal structure in the area of Deception Island, West Antarctica, which were made during the Polish Antarctic Geodynamical Expeditions in 1979-80 and 1987-88. In the caldera and immediate vicinity of Deception Island a layer of unconsolidated and poorly consolidated young sediments of 1.9–2.2 km s−1 P-wave velocity was found. Velocities of 4.1–4.3 km s−1 were found in the depth interval from 0.6–1.3 to about 3 km. Lateral differences in upper crustal structure between the south-eastern and western sectors were

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Navarro, F. J., J. Otero, Yu Ya Macheret, et al. "Radioglaciological studies on Hurd Peninsula glaciers, Livingston Island, Antarctica." Annals of Glaciology 50, no. 51 (2009): 17–24. http://dx.doi.org/10.3189/172756409789097603.

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AbstractWe present the results of several radio-echo sounding surveys carried out on Johnsons and Hurd Glaciers, Livingston Island, Antarctica, between the 1999/2000 and 2004/05 austral summer campaigns, which included both radar profiling and common-midpoint measurements with low (20– 25 MHz)- and high (200 MHz)-frequency radars. The latter have allowed us to estimate the radio-wave velocity in ice and firn and the corresponding water contents in temperate ice, which vary between 0 and 1.6% depending on the zone. Maximum ice thickness is ~200 m, with a mean value of 93.6±2.5 m. Total ice volu

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Pallàs, R., J. M. Vilaplana, and F. Sàbat. "Geomorphological and neotectonic features of Hurd Peninsula, Livingston Island, South Shetland Islands." Antarctic Science 7, no. 4 (1995): 395–406. http://dx.doi.org/10.1017/s0954102095000551.

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On Hurd Peninsula (Livingston Island) neotectonic features, such as faults, affect the landforms and emerged marine levels. A detailed local study of these features provides information on the recent structural and geomorphological evolution of the area. We suggest that Hurd Peninsula is divided into several tectonic blocks separated by faults. Movement of the faults determines the relative altitude of these blocks and, in consequence, their susceptibility to glacial, periglacial or marine processes. Although some of the tectonic movements reflected in the landforms may have been inherited fro

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Gil-Delgado, J. A., J. González-Solís, and A. Barbosa. "Populations of breeding birds in Byers Peninsula, Livingston Island, South Shetland Islands." Antarctic Science 25, no. 2 (2013): 303–6. http://dx.doi.org/10.1017/s0954102012000752.

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AbstractData about breeding populations of birds in the Antarctica are rare and fragmented. Thus, information about the status of the breeding populations of Antarctic birds is crucial given the current scenario of climate change, which is particularly acute in Antarctica. This paper presents new information about the populations of the Antarctic tern Sterna vittata, the kelp gull Larus dominicanus, the southern giant petrel Macronectes giganteus, the Antarctic skua Catharacta antarctica lonnbergi, the chinstrap penguin Pygoscelis antarctica and the gentoo penguin Pygoscelis papua on Byers Pen

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Cruwys, E., and Pamela B. Davis. "Southern elephant seal numbers during moult on Livingston Island, South Shetland Islands." Polar Record 30, no. 175 (1994): 313–14. http://dx.doi.org/10.1017/s0032247400024591.

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Van de Vijver, Bart, Janelle T. Agius, John A. E. Gibson, and Antonio Quesada. "AN UNUSUAL SPINE-BEARINGPINNULARIASPECIES FROM THE ANTARCTIC LIVINGSTON ISLAND (SOUTH SHETLAND ISLANDS)." Diatom Research 24, no. 2 (2009): 431–41. http://dx.doi.org/10.1080/0269249x.2009.9705812.

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Zidarova, Ralitsa, Myriam De Haan, Plamen Ivanov, Elitsa Hineva, and Bart Van De Vijver. "The genus Craspedostauros E.J.Cox (Bacillariophyta) on the coasts of Livingston Island, Maritime Antarctica." Phytotaxa 572, no. 1 (2022): 1–24. https://doi.org/10.11646/phytotaxa.572.1.1.

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Zidarova, Ralitsa, Haan, Myriam De, Ivanov, Plamen, Hineva, Elitsa, Vijver, Bart Van De (2022): The genus Craspedostauros E.J.Cox (Bacillariophyta) on the coasts of Livingston Island, Maritime Antarctica. Phytotaxa 572 (1): 1-24, DOI: 10.11646/phytotaxa.572.1.1, URL: http://dx.doi.org/10.11646/phytotaxa.572.1.1

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Pimpirev, Christo, Marin Ivanov, Dimo Dimov, and Todor Nikolov. "First find of the Upper Tithonian ammonite genus Blanfordiceras from the Miers Bluff Formation, Livingston Island, South Shetland Islands." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2002, no. 6 (2002): 377–84. http://dx.doi.org/10.1127/njgpm/2002/2002/377.

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Lyons, W. Berry, K. A. Welch, S. A. Welch, et al. "Geochemistry of streams from Byers Peninsula, Livingston Island." Antarctic Science 25, no. 2 (2013): 181–90. http://dx.doi.org/10.1017/s0954102012000776.

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AbstractIn January and February 2009, a series of water samples were collected from streams on Byers Peninsula. These samples were analysed for major elements and δ18O to determine the role of lithology and landscape position on stream geochemistry, and to understand better the hydrology (i.e. residence time of water) of these systems. Precipitation chemistry is enriched in Na+, as are the streams located close to the coast. Streams originating from inland locations have much higher percentages of Ca2+. In contrast, Mg2+ varied little, though streams that are in greater contact with volcanic-d

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Ximenis, L., J. Calvet, D. Garcia, J. M. Casas, and F. Sàbat. "Folding in the Johnsons Glacier, Livingston Island, Antarctica." Geological Society, London, Special Publications 176, no. 1 (2000): 147–57. http://dx.doi.org/10.1144/gsl.sp.2000.176.01.11.

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Warren, Joseph D., and David A. Demer. "Near‐shore krill distribution around Livingston Island, Antarctica." Journal of the Acoustical Society of America 115, no. 5 (2004): 2557. http://dx.doi.org/10.1121/1.4809283.

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Smellie, John L. "Chapter 3.2a Bransfield Strait and James Ross Island: volcanology." Geological Society, London, Memoirs 55, no. 1 (2021): 227–84. http://dx.doi.org/10.1144/m55-2018-58.

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AbstractFollowing more than 25 years of exploration and research since the last regional appraisal, the number of known subaerially exposed volcanoes in the northern Antarctic Peninsula region has more than trebled, from less than 15 to more than 50, and that total must be increased at least three-fold if seamounts in Bransfield Strait are included. Several volcanoes remain unvisited and there are relatively few detailed studies. The region includes Deception Island, the most prolific active volcano in Antarctica, and Mount Haddington, the largest volcano in Antarctica. The tectonic environmen

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Krause, Douglas J., Michael E. Goebel, Greg J. Marshall, and Kyler Abernathy. "Summer diving and haul-out behavior of leopard seals (Hydrurga leptonyx) near mesopredator breeding colonies at Livingston Island, Antarctic Peninsula." Marine Mammal Science 32, no. 3 (2016): 839–67. https://doi.org/10.1111/mms.12309.

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Krause, Douglas J., Goebel, Michael E., Marshall, Greg J., Abernathy, Kyler (2016): Summer diving and haul-out behavior of leopard seals (Hydrurga leptonyx) near mesopredator breeding colonies at Livingston Island, Antarctic Peninsula. Marine Mammal Science 32 (3): 839-867, DOI: 10.1111/mms.12309, URL: http://dx.doi.org/10.1111/mms.12309

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Lonin, Serguei, Wilson A. Rios-Angulo, and Jairo Coronado. "Swell Conditions at Potential Sites for the Colombian Antarctic Research Station." Sustainability 14, no. 4 (2022): 2318. http://dx.doi.org/10.3390/su14042318.

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The objective of this paper was to characterize swell conditions in the coastal zone of the South Shetland Islands, where our preliminary analyses evaluated potential locations for the Colombian scientific station. The Simulating Waves Nearshore (SWAN) spectral model was implemented for the Bransfield Strait. The boundary conditions were selected by a cluster analysis of the wave climate from global hindcasting obtained with the WAVEWATCH III model. Some comparisons between the model and wavemeter measurements were made. The results demonstrated that optimal sea state conditions for the scient

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Martinez, Laura Lopez. "San Andres, a Herstory, or Writing Caribbean History from the Margins." Women, Gender, and Families of Color 9, no. 2 (2021): 230–44. http://dx.doi.org/10.5406/23260947.9.2.07.

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Abstract The island of San Andrés is located approximately 110 miles east of the Caribbean coast of Nicaragua and 300 miles west-northwest of the Colombian mainland. The literature and culture of the islands in the San Andrés and Providencia archipelago are still not very well known or studied, both within and outside Colombia, due to problems in editorial work, translation, and distribution and also because the relationship between the mainland and the islands has been often tense and difficult. The article will examine the 1987 novel San Andres, a Herstory by Keshia Howard-Livingston from th

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Smellie, J. L., M. Liesa, J. A. Muñoz, F. Sàbat, R. Pallàs, and R. C. R. Willan. "Lithostratigraphy of volcanic and sedimentary sequences in central Livingston Island, South Shetland Islands." Antarctic Science 7, no. 1 (1995): 99–113. http://dx.doi.org/10.1017/s0954102095000137.

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Livingston Island contains several, distinctive sedimentary and volcanic sequences, which document the history and evolution of an important part of the South Shetland Islands magmatic arc. The turbiditic, late Palaeozoic–early Mesozoic Miers Bluff Formation (MBF) is divided into the Johnsons Dock and Napier Peak members, which may represent sedimentation in upper and lower mid-fan settings, respectively, prior to pre-late Jurassic polyphase deformation (dominated by open folding). The Moores Peak breccias are formed largely of coarse clasts reworked from the MBF. The breccias may be part of t

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Tokarski, Antoni K., and Marek Doktor. "Lithostratigraphy of volcanic and sedimentary sequences in central Livingston Island, South Shetland Islands." Antarctic Science 8, no. 2 (1996): 207. http://dx.doi.org/10.1017/s0954102096210272.

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Willan, Robert C. R., John L. Smellie, Francesc Sàbat, and Josep A. Muñoz. "Lithostratigraphy of volcanic and sedimentary sequences in central Livingston Island, South Shetland Islands." Antarctic Science 8, no. 2 (1996): 207–8. http://dx.doi.org/10.1017/s0954102096220279.

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Jigena, Bismarck, Manuel Berrocoso, Cristina Torrecillas, Juan Vidal, Ignacio Barbero, and Alberto Fernandez-Ros. "Determination of an experimental geoid at Deception Island, South Shetland Islands, Antarctica." Antarctic Science 28, no. 4 (2016): 277–92. http://dx.doi.org/10.1017/s0954102015000681.

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AbstractDeception Island is an active volcano located in Bransfield Strait. Its volcanic activity is linked to the presence of gravity anomalies that influence the definition of the geoid. In this paper, a precise undulation geoid model (GeoiDEC14) has been computed from GPS, gravimetric and levelling measurements. GeoiDEC14 highlights local anomalies of the island that match with hot spots, such as the minimum values shown in Fumarole Bay and Whalers Bay (fumarole areas), or the maximum values found in the remains of lava at Colatinas, Black Glacier and Murature Point. Comparison of GeoiDEC14

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Nielsen, Uffe N., Diana H. Wall, Grace Li, Manuel Toro, Byron J. Adams, and Ross A. Virginia. "Nematode communities of Byers Peninsula, Livingston Island, maritime Antarctica." Antarctic Science 23, no. 4 (2011): 349–57. http://dx.doi.org/10.1017/s0954102011000174.

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AbstractThe nematode communities of Antarctica are considered simple. The few species present are well adapted to the harsh conditions and often endemic to Antarctica. Knowledge of Antarctic terrestrial ecosystems is increasing rapidly, but nematode communities remain to be explored in large parts of Antarctica. In soil samples collected at Byers Peninsula (Antarctic Specially Protected Area No. 126), Livingston Island we recorded 37 nematode taxa but samples showed great variation in richness and abundance. Nematode richness decreased with increasing soil pH, whereas total abundances, and the

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Acevedo, Jorge, Anelio Aguayo-Lobo, and Daniel Torres. "Albino Weddell seal at Cape Shirreff, Livingston Island, Antarctica." Polar Biology 32, no. 8 (2009): 1239–43. http://dx.doi.org/10.1007/s00300-009-0680-8.

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Hall, Kevin. "Some observations regarding sorted stripes, livingston island, south shetlands." Permafrost and Periglacial Processes 5, no. 2 (1994): 119–26. http://dx.doi.org/10.1002/ppp.3430050206.

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