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Calcareous Nannofossils - Science topic

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I attached the soil analysis to this question, I have never seen a soil with as much as 90% Calcium saturation. In these conditions, what should I pay attention to please when adding fertilizers. I realize that micros will certainly be an issue due to the pH.
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The concerned soil seems like calcareous in nature. Surprisingly , soil test values for P so high ,even Fe is good enough . Application of sulfur would be agood strategy to solubilise some calcium carbonate to netralise the soil pH. Have you separated CEC for calcium carbonate versus soil texture..??
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Soil test is attached, main concerns are tremendous amounts of calcium and very high pH.
I have access to DAP/TSP and the more expensive commercial P2O5 fertilizers.
I read that TSP may have an acidification effect, but will the 15% Ca add more of an already overloaded thing?
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Dear all,
I am working on the biostratigraphy of Pleistocene sediments from the high latitude region in south-east Indian ocean sediments. Kindly suggest me any book or articles in which the above-mentioned foraminifera are discussed. The articles on the zonation will more be appreciated.
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These species have been seen along with possible Calpionellids and possible Saccocoma fragments
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Yes, these microfossils look like calcispheres.
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I have some Eocene samples characterized by planktonic foraminifera assemblages ( I.e.Clavigerinella colombiana, Clavigerinella akersi,and Pseudoglobigerinella bolivariana), which are better adapted to eutrotrophic cold water environments. At the same time in such samples I find increased abundance of calcareous nannofossil genus Chiasmolithos.
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In view of recent researches, earlier markers of Calcareous Nannofossils defining Turonian-Coniacian Boundary are no more tenable. Is it possible now to demarcate Turonian-Coniacian Boundary by exclusive use of Calcareous Nannofossils? 
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Sorry - no contradiction; I didn't have my book chapter to hand and that's the Con-Sant boundary that falls in UC11c. The Tur-Con boundary does indeed fall in UC9c, between base Broinsonia parca expansa (older) and base Micula staurophora (younger) - and M. staurophora is globally abundant soon after its base. As for the boundary marker being an inoceramid - do not underestimate the amount of work that has been carried out on various potential candidate sections, looking for the best section and best marker for the boundary. I have been working with a number of people on these sections for nearly 30 years! No section and no boundary event will ever be perfect, but having a GSSP to refer to is absolutely necessary to fix the boundary, so that all other works can refer to that fixed point. Otherwise, we would only ever have a 'floating' age-model, and every fossil group would have its own idea of the boundary, but these wouldn't directly correlate. Given this, you won't find a nanno marker that 'delineates' the boundary, because none falls at the proposed boundary, but you can bracket the boundary using nannos, and that is the precise way boundary biostrat works, that lends itself to precise correlation.
As for there being no documentation of the nannos around the Tur-Con boundary (apart from the book chapter, which synthesises a lot of work, and the paper I mentioned yesterday), one problem is that these are short stages and there are very few sections to examine, but see:
2008    Lees, J.A. The calcareous nannofossil record across the Late Cretaceous Turonian/Coniacian boundary, including new data from Germany, Poland, the Czech Republic and England. Cretaceous Research, 29: 40-64. doi:10.1016/j.cretres.2007.08.002 
I don't know if you're aware that Nannotax3 (http://ina.tmsoc.org/Nannotax3/index.html) is a free online nannofossil taxonomy database, the primary aim of which is to standardise nannofossil taxonomy...
I don't understand how you're applying biostrat to your section - (1) if it's non-marine, it's likely any nannos were washed in from deposits, (2) and if these are really marine incursions, then you look for markers and work out what age you have from what's present (or absent).
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The object (more objects) was found in the examination of of calcareous nannofossils in the Lower - Middle Jurassic sediments. It can be a part of the nannoplankton body. Thank you for your help :-)
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Can you upload the image of higher size?
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I have found some grains in the Middle Triassic carbonates (Lower Anisian, Aegean, Lower Muschelkalk) and I'm trying to identify them - please see the attached pictures.
Are they calcispheres of algal origin (e.g., Globochaete alpina) ?
Is it possible to identity them in a range of genus, species?
Does anyone have any experience with such objects?
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Dear Monika,
Because your question was formulated: “Middle Triassic calcispheres?” I answered in this connection. On closer examination of attached photos, I turned my attention to the pictures 4 and 7. They resemble the sections of the species Gemeridella minuta Borza & Misik. I hope that for you in this case could be useful following articles:
1. Borza, K., Misik, M. 1975. Gemeridella minuta n. gen., n. sp. aus der oberen Trias der Westkarpaten. Geol. Zb., 26; 77-81.
2. Misik, M., Borza, K., 1978. Gemeridella, Didemnoides, Didemnum und Korperchen ahnlicher Gestalt aus dem Mesozoikum der Westkarpaten. Geol. Zb.– Geologica Carpathica, 29; 307–326.
Good luck!
Daria