nannoplankton sentence in Hindi
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- Coccoliths and related fossils are referred to as " calcareous nannofossils " or " calcareous nannoplankton ".
- The base of the Bartonian is at the first appearance of the calcareous nannoplankton species " Reticulofenestra reticulata ".
- The base of the Tortonian stage is at the last common appearance of calcareous nannoplankton " Globigerinoides subquadratus ".
- The base of the Serravallian is at the first occurrence of fossils of the nannoplankton species " Sphenolithus heteromorphus " and is located in the magnetic chronozone C5ABr.
- The base of the Priabonian stage is at the first appearance of calcareous nannoplankton species " Chiasmolithus oamaruensis " ( which forms the base of nannoplankton biozone NP18 ).
- The base of the Priabonian stage is at the first appearance of calcareous nannoplankton species " Chiasmolithus oamaruensis " ( which forms the base of nannoplankton biozone NP18 ).
- The gradual replacement of the radiolarian oozes of the Ruhpolding Formation by coccolith oozes of the overlying Aptychen Beds can be explained by further deepening of the basin and / or by blooming calcareous nannoplankton.
- Nano, with a single " n " in the middle, is a prefix meaning one-billionth, but geologists use a variant spelling in their word for the tiny ocean creatures called nannoplankton.
- The top of the Bartonian stage ( the base of the Priabonian ) is at the first appearance of calcareous nannoplankton species " Chiasmolithus oamaruensis " ( which forms the base of nannoplankton biozone NP18 ).
- The top of the Bartonian stage ( the base of the Priabonian ) is at the first appearance of calcareous nannoplankton species " Chiasmolithus oamaruensis " ( which forms the base of nannoplankton biozone NP18 ).
- The top of the Langhian stage ( the base of the Serravallian stage ) is at the first occurrence of fossils of the nannoplankton species " Sphenolithus heteromorphus " and is located in magnetic chronozone C5ABr.
- The top of the Maastrichtian stage is defined to be at the iridium anomaly at the Cretaceous Paleogene boundary ( K Pg boundary ), which is also characterised by the extinction of many groups of life, such as certain foraminifers and calcareous nannoplankton, all ammonites and belemnites, etc.
- The top of the Chattian stage ( which is the base of the Aquitanian stage, Miocene series and Neogene system ) is at the first appearance of foram species " Paragloborotalia kugleri ", the extinction of calcareous nannoplankton species " Reticulofenestra bisecta " ( which forms the base of nannoplankton biozone NN1 ), and the base of magnetic C6Cn . 2n.
- The top of the Chattian stage ( which is the base of the Aquitanian stage, Miocene series and Neogene system ) is at the first appearance of foram species " Paragloborotalia kugleri ", the extinction of calcareous nannoplankton species " Reticulofenestra bisecta " ( which forms the base of nannoplankton biozone NN1 ), and the base of magnetic C6Cn . 2n.
- The base of the Aquitanian ( also the base of the Miocene system ) is defined as the place in the stratigraphic column at the first appearance of foram species " Paragloborotalia kugleri ", the extinction of calcareous nannoplankton species " Reticulofenestra bisecta " ( which forms the base of nannoplankton biozone NN1 ), and the base of magnetic chronozone C6Cn . 2n.
- The base of the Aquitanian ( also the base of the Miocene system ) is defined as the place in the stratigraphic column at the first appearance of foram species " Paragloborotalia kugleri ", the extinction of calcareous nannoplankton species " Reticulofenestra bisecta " ( which forms the base of nannoplankton biozone NN1 ), and the base of magnetic chronozone C6Cn . 2n.
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