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L R Stevens

Dados Biográficos

ID11047269
NOMEL R Stevens
PRENOMESL R
SOBRENOMEStevens
ASSINATURASTEVENS L R
AFILIAÇÕESDepartment of Geosciences, University of Nebraska, Lincoln, NE 68588-0340, Nebraska, USA
VERIFICADONão
TOTAL DE OBRAS1
TOTAL DE CITAÇÕES17
TOTAL COMO AUTOR1
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO2001
ANO MAIS RECENTE DE PUBLICAÇÃO2001
ÍNDICE H1
  • Proposed changes in seasonality of climate during the Lateglacial and Holocene at Lake Zeribar, Iran

    Open Access•Lora Stevens, L R Stevens et al.•ARTICLE•The Holocene•2001•Citada por: 17•Referências: 11

    Calcareous sediments spanning the last 13 ka from Lake Zeribar, western Iran, were sampled for stable-isotope analysis as a means of augmenting earlier climatic interpretations based on pollen and macrofossils. The Lateglacial period was cold and dry, supporting semi-desert vegetation and highly concentrated lake water. Low evaporation rates due to the cold resulted in long residence times and high lake stands. Durinig the early Holocene, the upl…

  • Proposed changes in seasonality of climate during the Lateglacial and Holocene at Lake Zeribar, Iran

    Open Access•Lora Stevens, L R Stevens et al.•ARTICLE•The Holocene•2001•Citada por: 17•Referências: 11

    Calcareous sediments spanning the last 13 ka from Lake Zeribar, western Iran, were sampled for stable-isotope analysis as a means of augmenting earlier climatic interpretations based on pollen and macrofossils. The Lateglacial period was cold and dry, supporting semi-desert vegetation and highly concentrated lake water. Low evaporation rates due to the cold resulted in long residence times and high lake stands. Durinig the early Holocene, the upl…

  • Proposed changes in seasonality of climate during the Lateglacial and Holocene at Lake Zeribar, Iran

    Open Access•Lora Stevens, L R Stevens et al.•ARTICLE•The Holocene•2001•Citada por: 17•Referências: 11

    Calcareous sediments spanning the last 13 ka from Lake Zeribar, western Iran, were sampled for stable-isotope analysis as a means of augmenting earlier climatic interpretations based on pollen and macrofossils. The Lateglacial period was cold and dry, supporting semi-desert vegetation and highly concentrated lake water. Low evaporation rates due to the cold resulted in long residence times and high lake stands. Durinig the early Holocene, the upl…

Archaeology and ancient environmental studies (1 obras) · Arid (1 obras) · Climatology (1 obras) · Ecology (1 obras) · Environmental Science (1 obras) · Evapotranspiration (1 obras) · Geography (1 obras) · Geology (1 obras) · Geology and Paleoclimatology Research (1 obras) · Geomorphology (1 obras)

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