Publications

10465 to 10476 of 14011 results

1. Neohyadesia microtricha (Acari: Astigmata: Algophagidae): a new species from the sub-Antarctic

   The sub-antarctic mite genus Neohyadesia (Acari: Astigmata) is known from two described taxa: N. signyi from Signy Island (South Orkney Islands, South Atlantic Province), and a subspecies, N. s. punctulata […]

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2. Milnesium cfr. tardigradum (Milnesiidae, Apochela, Tardigrada): a monitor of high altitude meiofauna on sub-Antarctic Marion Island

   The meiofaunal tardigrades Milnesium cfr. tardigradum, Echiniscus sp., and Macrobiotus sp. were extracted from high altitude moss and volcanic scoria samples on sub-Antarctic Marion Island. Gut contents of mounted Milnesium […]

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3. Is it real?

   How true is the statement: “The camera never lies”? Trick photography has a long and varied history, and good fakes are extremely difficult to refute. Now computer software makes it […]

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4. Global Collembola on Deception Island

   Three new non-indigenous springtail species are recorded in recent collections made on Deception Island, South Shetland Islands, maritime Antarctic: Deuteraphorura (Deuteraphorura) cebennaria (Gisin) (Collembola: Onychiuridae), Mesaphorura macrochaeta Rusek (Tullbergiidae), and […]

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5. On self-similar and multifractal models for the scaling of extreme bursty fluctuations in space plasmas

   Read more of: On self-similar and multifractal models for the scaling of extreme bursty fluctuations in space plasmas

6. Marine and terrestrial environmental changes in NW Europe preceding carbon release at the Paleocene-Eocene transition

   Environmental changes associated with the Paleocene–Eocene thermal maximum (PETM, ∼56 Ma) have not yet been documented in detail from the North Sea Basin. Located within proximity to the North Atlantic […]

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7. The 4th PAGES Past Interglacials Workshop. Department of Earth Sciences, University of Cambridge, Cambridge, UK, 2-5 July 2012

   Read more of: The 4th PAGES Past Interglacials Workshop. Department of Earth Sciences, University of Cambridge, Cambridge, UK, 2-5 July 2012

8. Long-range transport of pollutants to the Falkland Islands and Antarctica: evidence from lake sediment fly ash particle records

   210Pb-dated sediment cores taken from lakes on the Falkland Islands, the South Orkney Islands, and the Larsemann Hills in Antarctica were analyzed for fly ash particles to assess the temporal […]

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9. A predominant reversal in the relationship between the SAM and East Antarctic temperatures during the Twenty-First Century

   The scientific literature portrays a temporally invariant spatial relationship between the phase of the southern annular mode (SAM) and the sign of surface air temperature (SAT) anomalies across Antarctica. However, […]

   Read more of: A predominant reversal in the relationship between the SAM and East Antarctic temperatures during the Twenty-First Century

10. Surface undulations of Antarctic ice streams tightly controlled by bedrock topography

    Full Stokes flow-line models predict that fast-flowing ice streams transmit information about their bedrock topography most efficiently to the surface for basal undulations with length scales between 1 and 20 […]

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11. Developing integrated models of Southern Ocean food webs: including ecological complexity, accounting for uncertainty and the importance of scale

    The Southern Ocean supports diverse and unique ecosystems that have been impacted by more than two centuries of exploitation and are now experiencing rapid changes in ocean temperature and seasonal […]

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12. High resolution reconstruction of Southwest Atlantic sea-ice and its role in the carbon cycle during marine isotope stages 3 and 2

    Recent modeling suggests that changes in Southern Ocean sea-ice extent potentially regulated the exchange of CO2 release between the ocean and atmosphere during glacials. Unfortunately, a lack of high-resolution sea-ice […]

    Read more of: High resolution reconstruction of Southwest Atlantic sea-ice and its role in the carbon cycle during marine isotope stages 3 and 2