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The Djupadal Formation is a geologic formation in Skåne County, southern Sweden. It is Early Jurassic (probably Pliensbachian-Toarcian, or Late Toarcian) in age. It is part of the Central Skåne Volcanic Province, know by the discovery of basalt tuff layers, including , and Djupadal. An original analysis of the location of Korsaröd led to a Toarcian-Aalenian age, but was dismissed in 2016, when a series of Palynogical samples recovered a Late Pliensbachian and probably Lower Toarcian age for the Korsaröd Outcrop. The same year this result was also challenged by an in-depth study of the Lilla Hagstad neck that yield a Late Toarcian Age. The formation was deposited in the Central Skane region, linked to the late early Jurassic volcanism. The Korsaröd member includes a volcanic-derived Lagers

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dbo:abstract
  • The Djupadal Formation is a geologic formation in Skåne County, southern Sweden. It is Early Jurassic (probably Pliensbachian-Toarcian, or Late Toarcian) in age. It is part of the Central Skåne Volcanic Province, know by the discovery of basalt tuff layers, including , and Djupadal. An original analysis of the location of Korsaröd led to a Toarcian-Aalenian age, but was dismissed in 2016, when a series of Palynogical samples recovered a Late Pliensbachian and probably Lower Toarcian age for the Korsaröd Outcrop. The same year this result was also challenged by an in-depth study of the Lilla Hagstad neck that yield a Late Toarcian Age. The formation was deposited in the Central Skane region, linked to the late early Jurassic volcanism. The Korsaröd member includes a volcanic-derived Lagerstatten with exceptional fern finds. The data provided by fossilized wood rings showed that the location of Korsaröd hosted a middle-latitude Mediterranean-type biome in the late Early Jurassic, with low rainfall ratio, delayed to seasonal events. Superimposed on this climate were the effects of a local active and hydrothermal activity. (en)
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dbp:age
  • Latest Pliensbachian- Latest Toarcian (en)
  • ~(A Volcanic neck suggest 176.7 ± 0.5 Ma, Late Toarcian Age) (en)
dbp:align
  • right (en)
dbp:caption
  • 600.0
dbp:footer
  • 3.15576E8
dbp:image
  • 0 (xsd:integer)
  • Marble Terrace in Waimangu Volcanic Valley.jpg (en)
  • Puy de Pariou 2001-07-30.jpg (en)
  • Puy de mercoeur dome.jpg (en)
dbp:mapCaption
  • Korsaröd Lagerstätten Location (en)
dbp:name
  • Djupadal Formation (en)
dbp:namedby
  • Carita Augustsson (en)
dbp:namedfor
  • Djupadalsmölla, Ljungbyhed (en)
dbp:otherlithology
  • Sandstone, Clay and Conglomerate (en)
dbp:overlies
  • Höör Sandstone, Brandsberga and Kolleberga erratics and Sapropel at Sandåkra (en)
dbp:paleocoordinates
  • Approx. 35°N (en)
dbp:period
  • Toarcian (en)
dbp:perrow
  • 2 (xsd:integer)
dbp:prilithology
  • Basalt Tuff, Veined Gneiss (en)
dbp:region
  • Central Skåne County (en)
dbp:subunits
  • Sapropel at Sandåkra (en)
dbp:thickness
  • Up to (en)
dbp:totalWidth
  • 350 (xsd:integer)
dbp:type
dbp:underlies
  • Cuaternary Sediments (en)
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  • The Djupadal Formation is a geologic formation in Skåne County, southern Sweden. It is Early Jurassic (probably Pliensbachian-Toarcian, or Late Toarcian) in age. It is part of the Central Skåne Volcanic Province, know by the discovery of basalt tuff layers, including , and Djupadal. An original analysis of the location of Korsaröd led to a Toarcian-Aalenian age, but was dismissed in 2016, when a series of Palynogical samples recovered a Late Pliensbachian and probably Lower Toarcian age for the Korsaröd Outcrop. The same year this result was also challenged by an in-depth study of the Lilla Hagstad neck that yield a Late Toarcian Age. The formation was deposited in the Central Skane region, linked to the late early Jurassic volcanism. The Korsaröd member includes a volcanic-derived Lagers (en)
rdfs:label
  • Djupadal Formation (en)
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