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  • 2005-2009  (582)
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  • 1
    Call number: IASS 16.90547
    Type of Medium: Monograph available for loan
    Pages: XLV, 448 S , Ill., graph. Darst., Kt
    ISBN: 9780660197241 , 0660197243 , 9781845935832 (CABI) , 1845935837 (CABI)
    Language: English
    Branch Library: RIFS Library
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  • 2
    Publication Date: 2024-01-09
    Keywords: 189-1171; Abundance per unit mass; COMPCORE; Composite Core; DEPTH, sediment/rock; Facies name/code; Factor 1; Factor 2; Factor 4; Factor 5; Foraminifera, planktic/benthic ratio; Joides Resolution; Leg189; Ocean Drilling Program; ODP; Size fraction 500.000-466.516 µm, 1.0-1.1 phi; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 200 data points
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  • 3
    Publication Date: 2024-01-09
    Keywords: 189-1171; Calculated; Comment; COMPCORE; Composite Core; DEPTH, sediment/rock; Facies name/code; Foraminifera; Joides Resolution; Leg189; Number of species; Ocean Drilling Program; ODP; Percentage; South Pacific Ocean; Species
    Type: Dataset
    Format: text/tab-separated-values, 372 data points
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  • 4
    Publication Date: 2024-01-09
    Keywords: 189-1171; Age, dated; Age, maximum/old; Age, minimum/young; Chronozone; COMPCORE; Composite Core; DEPTH, sediment/rock; Depth comment; Isotopic event; Joides Resolution; Leg189; Lithologic unit/sequence; Ocean Drilling Program; ODP; South Pacific Ocean; Type; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Myers-Smith, Isla H; Harden, J W; Wilmking, Martin; Fuller, C C; McGuire, A David; Chapin, F Stuart (2008): Wetland succession in a permafrost collapse: interactions between fire and thermokarst. Biogeosciences, 5(5), 1273-1286, https://doi.org/10.5194/bg-5-1273-2008
    Publication Date: 2023-12-13
    Description: To determine the influence of fire and thermokarst in a boreal landscape, we investigated peat cores within and adjacent to a permafrost collapse feature on the Tanana River Floodplain of Interior Alaska. Radioisotope dating, diatom assemblages, plant macrofossils, charcoal fragments, and carbon and nitrogen content of the peat profile indicate ~600 years of vegetation succession with a transition from a terrestrial forest to a sedge-dominated wetland over 100 years ago, and to a Sphagnum-dominated peatland in approximately 1970. The shift from sedge to Sphagnum, and a decrease in the detrended tree-ring width index of black spruce trees adjacent to the collapse coincided with an increase in the growing season temperature record from Fairbanks. This concurrent wetland succession and reduced growth of black spruce trees indicates a step-wise ecosystem-level response to a change in regional climate. In 2001, fire was observed coincident with permafrost collapse and resulted in lateral expansion of the peatland. These observations and the peat profile suggest that future warming and/or increased fire disturbance could promote permafrost degradation, peatland expansion, and increase carbon storage across this landscape; however, the development of drought conditions could reduce the success of both black spruce and Sphagnum, and potentially decrease the long-term ecosystem carbon storage.
    Keywords: Alaska, USA; International Polar Year (2007-2008); IPY; PERM; Sampling permafrost; Tanana_R-plain
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
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    PANGAEA
    In:  Supplement to: Pekar, Stephen F; Hucks, Audrey; Fuller, Michael D; Li, Shawna (2005): Glacioeustatic changes in the early and middle Eocene (51-42 Ma): Shallow-water stratigraphy from ODP Leg 189 Site 1171 (South Tasman Rise) and deep-sea d18O records. Geological Society of America Bulletin, 117(7-8), 1081-1093, https://doi.org/10.1130/B25486.1
    Publication Date: 2024-01-09
    Description: Sequence boundary ages determined in shallow-water sediments obtained from ODP (Ocean Drilling Program) Leg 189 Site 1171 (South Tasman Rise) compare well with other stratigraphic records (New Jersey, United States, and northwestern Europe) and d18O increases from deep-sea records, indicating that significant (〉10 m) eustatic changes occurred during the early to middle Eocene (51-42 Ma). Sequence boundaries were identified and dated using lithology, bio- and magnetostratigraphy, water-depth changes, CaCO3 content, and physical properties (e.g., photospectrometry). They are characterized by a sharp bioturbated surface, low CaCO3 content, and an abrupt increase in glauconite above the surface. Foraminiferal biofacies and planktonic/benthic foraminiferal ratios were used to estimate water-depth changes. Ages of six sequence boundaries (50.9, 49.2, 48.5-47.8, 47.1, 44.5, and 42.6 Ma) from Site 1171 correlate well to the timings of d18O increases and sequence boundaries identified from other Eocene studies. The synchronous nature of sequence boundary development from globally distal sites and d18O increases indicates a global control and that glacioeustasy was operating in this supposedly ice-free world. This is supported by previous modeling studies and atmospheric pCO2 estimates showing that the first time pCO2 levels decreased below a threshold that would support the development of an Antarctic ice sheet occurred at ca. 51 Ma. Estimates of sea-level amplitudes range from ~20 m for the early Eocene (51-49 Ma) and ~25 m to ~45 m for the middle Eocene (48-42 Ma) using constraints established for Oligocene d18O records.
    Keywords: 189-1171; COMPCORE; Composite Core; Joides Resolution; Leg189; Ocean Drilling Program; ODP; South Pacific Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 7
    Publication Date: 2017-04-03
    Description: We assess the quality of the version 2.2 (v2.2) HNO3 measurements from the Microwave Limb Sounder (MLS) on the Earth Observing System Aura satellite. The MLS HNO3 product has been greatly improved over that in the previous version (v1.5), with smoother profiles, much more realistic behavior at the lowest retrieval levels, and correction of a high bias caused by an error in one of the spectroscopy files used in v1.5 processing. The v2.2 HNO3 data are scientifically useful over the range 215 to 3.2 hPa, with single-profile precision of 0.7 ppbv throughout. Vertical resolution is 3–4 km in the upper troposphere and lower stratosphere, degrading to 5 km in the middle and upper stratosphere. The impact of various sources of systematic uncertainty has been quantified through a comprehensive set of retrieval simulations. In aggregate, systematic uncertainties are estimated to induce in the v2.2 HNO3 measurements biases that vary with altitude between ±0.5 and ±2 ppbv and multiplicative errors of ±5–15% throughout the stratosphere, rising to ±30% at 215 hPa. Consistent with this uncertainty analysis, comparisons with correlative data sets show that relative to HNO3 measurements from ground-based, balloon-borne, and satellite instruments operating in both the infrared and microwave regions of the spectrum, MLS v2.2 HNO3 mixing ratios are uniformly low by 10–30% throughout most of the stratosphere. Comparisons with in situ measurements made from the DC-8 and WB-57 aircraft in the upper troposphere and lowermost stratosphere indicate that the MLS HNO3 values are low in this region as well, but are useful for scientific studies (with appropriate averaging).
    Description: Published
    Description: D24S40
    Description: 1.7. Osservazioni di alta e media atmosfera
    Description: JCR Journal
    Description: reserved
    Keywords: satellite validation ; stratospheric HNO3 ; 01. Atmosphere::01.01. Atmosphere::01.01.01. Composition and Structure
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2019-12-03
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 9
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    In:  Zoologische Mededelingen (00240672) vol.79-3 (2005) p.131
    Publication Date: 2007-01-16
    Description: Bird collections are an increasingly valuable resource for the scientific and artistic communities. A number of recommendations are made which should facilitate legitimate use of bird collections, and help to justify the continued support of these collections. 1. If staffing limitations hinder the legitimate use of an institution’s collections, this situation should be used as justification for better funding. 2. Online catalogues have a valuable but limited role in facilitating research; directors of institutions must be made aware that such catalogues do not diminish the role of the curatorial staff. 3. All stakeholders must accept their responsibility to prevent further marginalization of museum collections. 4. In many cases the value of having rare artefacts on public display is greater than the risk to those items, and so institutions should consider placing a greater proportion of their most valuable artefacts on display to the public. 5. Institutions should develop and publish guidelines on acceptable uses of their collections and a list of applicable fees if such fees are appropriate. These guidelines should include a description of the procedures involved in applying for access to the collection.
    Keywords: museum collections ; 42.83
    Repository Name: National Museum of Natural History, Netherlands
    Type: Article / Letter to the editor
    Format: application/pdf
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  • 10
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    WWF
    Publication Date: 2021-05-19
    Description: For most activities, a relatively low level of exertion is required. While the ship will sometimes dock for a dry landing, you will need to climb into and out of Zodiacs for certain excursions ashore and for some snorkeling and most diving activities. Staff and crew will be on hand to assist. On shore excursions, you must be able to walk moderate distances in villages, towns, forests, and on beaches, occasionally over rough terrain. Opportunities will be available for leisurely strolls, as well as optional hikes requiring more exertion. Birders may participate in ornithological excursions. Our expedition staff and renowned lecture team of naturalists and historians will accompany you throughout shore and afloat. Average daily temperatures will be in the 80s F, with the possibility of occasional afternoon showers. A complete list of recommended clothing, essentials to bring, and a suggested reading list will be mailed to you approximately four months prior to departure. Exact ship arrival times are often dependent upon winds and currents. Participants will most enjoy these remarkable destinations if they travel with a spirit of adventure and flexibility.
    Description: WWF
    Keywords: Oceans
    Repository Name: AquaDocs
    Type: Other
    Format: 1631709 bytes
    Format: application/pdf
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