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Elisabeth Alve

Biographic Data

ID6572358
NAMEElisabeth Alve
GIVEN NAMESElisabeth
FAMILY NAMEAlve
SIGNATUREALVE E
AFFILIATIONSUniversity of Oslo
ORCID0000-0001-6692-7800
VERIFIEDYes
TOTAL WORKS2
TOTAL CITATIONS4
WORKS AS AUTHOR2
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1991
LATEST PUBLICATION YEAR2017
H-INDEX1
  • Spatial and temporal organic carbon burial along a fjord to coast transect

    Open Access•C J Duffield, CJ Duffield et al.•ARTICLE•The Holocene•2017•References: 2

    We investigated spatial and temporal changes in accumulation rate and source of organic carbon on a gradient along the Lysefjord and the more coastal Høgsfjord, Western Norway. This was achieved through analysis of total organic carbon and nitrogen content of sediment cores, which were radiometrically dated to the early 19th and 20th centuries for the Høgsfjord and Lysefjord, respectively. Benthic foraminifera (protists) were utilized to determin…

  • Foraminifera, climatic change, and pollution

    Open Access•Elisabeth Alve•ARTICLE•The Holocene•1991•Cited by: 4•References: 2

    Benthic foraminifera are shown to reflect both natural (including climatic) and human- induced environmental alterations over the last 1500 years in Drammensfjord, Norway. Today, Drammensfjord is a 124 m deep, partly anoxic, hyposaline basin (salinity <32%o) separated from the adjoining Oslo Fjord by a sill at 10 m water depth. It has been affected by human-induced organic pollution for more than a century. Based on major faunal trends, sediment …

  • Foraminifera, climatic change, and pollution

    Open Access•Elisabeth Alve•ARTICLE•The Holocene•1991•Cited by: 4•References: 2

    Benthic foraminifera are shown to reflect both natural (including climatic) and human- induced environmental alterations over the last 1500 years in Drammensfjord, Norway. Today, Drammensfjord is a 124 m deep, partly anoxic, hyposaline basin (salinity <32%o) separated from the adjoining Oslo Fjord by a sill at 10 m water depth. It has been affected by human-induced organic pollution for more than a century. Based on major faunal trends, sediment …

  • Foraminifera, climatic change, and pollution

    Open Access•Elisabeth Alve•ARTICLE•The Holocene•1991•Cited by: 4•References: 2

    Benthic foraminifera are shown to reflect both natural (including climatic) and human- induced environmental alterations over the last 1500 years in Drammensfjord, Norway. Today, Drammensfjord is a 124 m deep, partly anoxic, hyposaline basin (salinity <32%o) separated from the adjoining Oslo Fjord by a sill at 10 m water depth. It has been affected by human-induced organic pollution for more than a century. Based on major faunal trends, sediment …

  • Spatial and temporal organic carbon burial along a fjord to coast transect

    Open Access•C J Duffield, CJ Duffield et al.•ARTICLE•The Holocene•2017•References: 2

    We investigated spatial and temporal changes in accumulation rate and source of organic carbon on a gradient along the Lysefjord and the more coastal Høgsfjord, Western Norway. This was achieved through analysis of total organic carbon and nitrogen content of sediment cores, which were radiometrically dated to the early 19th and 20th centuries for the Høgsfjord and Lysefjord, respectively. Benthic foraminifera (protists) were utilized to determin…

Benthic zone (2 works) · Foraminifera (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Isotope Analysis in Ecology (2 works) · Oceanography (2 works) · Anoxic waters (1 work) · Chemistry (1 work) · Climate change (1 work) · Ecology (1 work)

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