Jotnian
In north European
Overview
Jotnian sediments include quartz-rich sandstones, siltstones, arkose, shale and conglomerates.[3][4] The characteristic red colour of Jotnian sediments is due to their deposition in subaerial (e.g. non-marine) conditions.[5] Jotnian sediments are the oldest known sediments in the Baltic area that have not been subject to metamorphism.[4][5]
Their age is poorly constrained, but generally they are younger than the rapakivi granites and older than Postjotnian[note 2] diabases that intrude the sediments. This means that Jotnian sediments were deposited approximately 1600–1260 million years ago. Some Jotnian sediments are, however, younger than the diabases, meaning they can be younger than 1260 million years.[2] Jotnian sediments are usually assigned to the Riphean Stage of the Mesoproterozoic Era.[1][2] Jotnian sediments rests on what is known as Subjotnian[note 3] rocks which include weathered rapakivi granites and the Hogland Series.[6][7][8] Amantov and co-workers comments about the terms Jotnian and Postjotnian that:[2]
the terms should be interpreted as more descriptive (i.e. the diabase usually cuts the sandstone) than temporal (all the Jotnian sandstones not necessarily older than all the Postjotnian diabases).
At large scale, Jotnian sediments are classified as being part of a "quasiplatform" group of sediments of the
Distribution
Selection of outcrop localities mentioned in the text.There is evidence suggesting that Jotnian cover rocks or a Jotnian
Baltic Sea
Between Finland and Sweden Jotnian sediments are common in the
Finland
Muhos
Muhos in the northeastern Gulf of Bothnia is a site of Jotnian sediment occurrence.[2] At this location Jotnian sediments can be found within the Muhos Graben that has had a downward displacement of about one kilometre. The sediments in the Muhos Graben at the bottom are conglomerates and arkoses whose contact with the underlying metamorphic rocks constitute an unconformity. The pebbles of the conglomerate are made of schist and granite while the matrix is made of arkose. The bulk (90–80%) of the sequence of sediments is made up of siltstones and shales. The colour of the siltstones and shales vary from red and brown to grey to green. The siltstones and shales are intercalated with arkosic sandstone. The red arkosic sandstones of Muhos Graben are comparable to the ones of Satakunta. These sediments are of fluvial origin.[5]
Satakunta
Southern Satakunta near the shores of the