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it's from Upper Triassic - Lower Jurassic I record it with dinoflagellate species
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Hi
what is the size ?
What about leech eggs ?
marc
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Hello, I am a PhD student in sedimentology and biostratigraphy, and I have a fossil leaf specimen from a Jurassic-Cretaceous deposit. I would like to receive recommendations on fossil plants used in stratigraphy, especially the upper jurrasic and lower cretaceous. Additionally, if possible, could someone help me find specialists or relevant articles on Jurassic and Cretaceous fossil plants?
Thank you very much for your assistance!
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Dear Omar Omar Ait Haddou ,
I apologize, but I am not expert in paleontology, paleobotany. But your evaluations must be excellent for this, a good knowledge of the environment (paleoenvironment), which will only be available if you can imagine the development of your research area well. I read some Algerian articles. Based on these, it can be said that the tectonics of the Atlas Mountains is based on a rather erroneous view.
So take that into consideration. They can really help you if they have proper knowledge of your research area.
It is currently tectonically active. Interesting conclusions can be drawn.
I will be retired soon, and I would love to explore the area in my free time.
I have no money, I'm not demanding, but my geological advice could be valuable.
Regards,
Laszlo
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Dear Colleagues:
These papers are very old. If you have a copy, please share with me.
Kind regards.
Subhronil
List:
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Kapitza, A. A. New species of lower Cretaceous inoceramid from lower Priamur. 65-77. In: Poyarkova, Z.N. (ed.). Biostratigraphy of the south of the Far East (Phanerozoic). DVNTS AN SSSR, Vladivostok. 139 pp.
M. M. Astafieva. 1989. On the representatives of the genus Maitaia (Bivalvia). Paleontological Journal 23(3):11-19
Keller, S. (1982). Die Oberkreide der Sack-Mulde bei Alfeld (Cenoman-Unter-Coniac). Lithologic, Biostratigraphie und Inceramen. Geol. Jahrb., 64, 3-171.
Heinz, R. (1932). Aus der neue Systematik der Inoceramen. Mitteilungen aus dem Mineralogisch-Geologischen Staatsinstituts in Hamburg, 13, 1-26.
Marwick, J. (1953). Divisions and faunas of the Hokonui System (Triassic and Jurassic). Geological Survey of New Zealand, Palaeontological Bulletin, 21, 1-141.
Chen, J. (1987). Early Jurassic marine bivalves from Guangdong-Nanling district, southern China. Bulletin of Nanjing Institute of Geology and Palaeontology, Academia Sinica, 12, 23-94.
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would like to ask you about this thin section which I found in the Upper Jurassic of Algeria."
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Dasyclads..two species of Salpingoporella..one is annulata...sure that it is Upper Jurassic? What is the evidence?
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This question is for an updated paleogeographical reconstruction of the Atlas Gulf and assiociated landmasses in the Early Jurassic (Early Toarcian)
We know that this Paleozoic montane rangue was exposed on the EJ (Frizon de Lamotte et al., 2008), that was being pushed by two rift systems (the Tethyan Atlas rift in the north and the Atlantic rift in the west) and that there was an ongoing exhumation, that cutaround 7.5–10.5 km of crustal rocks by the end of the Middle Jurassic (Gouiza et al., 2017). As well there is evidence it was a source for siliclastic materials in the Early Jurassic Atlas Gulf (Krencker et al. 2020).
But, is there any suggested reconstrucion of it´s appperance? Or a suggestion of what it may have looked like?
-Frizon de Lamotte, D., Zizi, M., Missenard, Y., Hafid, M., Azzouzi, M. E., Maury, R. C., ... & Michard, A. (2008). The atlas system. Continental Evolution: The Geology of Morocco: Structure, Stratigraphy, and Tectonics of the Africa-Atlantic-Mediterranean Triple Junction, 133-202.
-Gouiza, M., Charton, R., Bertotti, G., Andriessen, P., & Storms, J. E. A. (2017). Post-Variscan evolution of the Anti-Atlas belt of Morocco constrained from low-temperature geochronology. International Journal of Earth Sciences, 106, 593-616.
-Krencker, F. N., Fantasia, A., Danisch, J., Martindale, R., Kabiri, L., El Ouali, M., & Bodin, S. (2020). Two-phased collapse of the shallow-water carbonate factory during the late Pliensbachian–Toarcian driven by changing climate and enhanced continental weathering in the Northwestern Gondwana Margin. Earth-Science Reviews, 208, 103254.
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I am not so familiar with the area you are researching. 27 years before I had to leave the profession... But since then I've been working in my former profession as a hobby... You should pay attention to what Ralph Thomas Becker said : 'The famous outcrop of Ouidane Chebbi and other Kem-Kem outcrops show a medium-scale hill and valley Devonian-Carboniferous topography transgressed by flat lying Cretaceous beds. So it seems that there was no alpine-style mountain range left in the Jurassic.'! Very logical!
If you look at his work he made paleontological study near the East of Anti-Atlas Range: Dra Walley... That is why you can use as prove his works... Regardless of that, without doing any research there - there is no possibility to do - my opinion was that the area worked as continental medium in Jurassic... You don't have an easy job... You need to do research in East (West Algeria, There has to exist drilling's Data! and seismic 3D surveys, 2D seismic sections) . In principle, you should be thinking about what the Moroccan Anti-Atlas would have looked like in the Early Jurassic nearly as it looks now... Only its West, North-West Area had other features. you have to determine correctly, why? I cannot say more about Hungary from here... It is clear what you have to do.
Regards,
Laszlo
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This is a Microphotogragh of Jurassic lacustrine shale in Sichuan basin.
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thanks for the news views
sorry it does not add much from wood point of view
it is a tracheidoxyl, i.e. a homoxylous wood, possibly that of a conifer
Apparently several shells get attached to this wood
see comments on the picture
you can use marc.philippeATuniv-lyon1.fr if you want to discuss further
marc
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These species probably belong to the subfamily Choffatellinae Maync, 1958 or family Spirocyclinidae Munier-Chalmas , 1887 (Image C1,C2) and family Hauraniidae Septfontaine, 1988 (Images C1 & C3).
Image C2 looks like to be Pseudocyclammina Yabe & Hanzawa, 1926
Imge C3 probably is Amijiella Loeblich & Tappan, 1985
Image C1 looks like Alzonella Bernier & Neumann, 1970 or any Cyclamminids but the network of chamberlets formed in the initial whorl is absent in other genera of this family (so far I know).
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фото сверху - это Rectocyclammina arrabidensis Remalho (кимеридж-берриас)
Фото слева снизу - Аlveosepta powersi (Redmond) (кимеридж)
справа снизу - Аlveosepta powersi (возможно)
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I´m looking for this work:
Krumbeck, L. (1932). Über den Fallaciosus-Horizont im Lias Mittel-ζ von Irlbach bei Regensburg. Centralblatt für Mineralogie, Geologie und Paläontologie 1932 (Abteilung B. Geologie und Paläontologie), 10, 499-518
Apparently, despite being focused on the Middle Liassic it also recovers the Progadation of Sandstones on the Lower Toarcian Locally (The "Dactyliocerassandstein"). And is one of the few works on this Outcrop of the Lias.
I ask if someone has this paper and can share it as PDF. Or know a place online where i can get it.
Thanks in advance
Antonio
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Thanks Harald! I will ask them.
all the best
Antonio
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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 already asked Dr Hisashi Suzuki and Dr Gawlick about the possibility of it being Radiolaria, However they both agreed it is not, though Dr Suzuki did not reject the possibility of it being new Radiolaria specie. It has been seen along with possible Calpionellids and possible Saccocoma fragments and Holothurians of Mesozoic.
I would be thankful to have new suggestions.
Thanks
Hesam
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Dear Hesam it is bryozoan fragment
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I can't identify these two bioclasts (yellow arrow)in the thin section I'm analyzing. The overall thin section is made up of angular to sub-rounded grains of feldspar with alterations, zonations and twinnings, opaques, lithics and quartz. The thin section was from an area believed to be Jurassic-Cretaceous Tembeling Group based on findings of poorly preserved horsetails in the area. The Tembeling Group is a continental deposit. But the bioclasts seem to be of marine in origin?
The three sections on the bioclast on the left got me thinking that it was a trilobite but I'm not sure. Or could it also be a foram?
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Dear Mrs. Azmi,
it is hard to judge which mineral(s) these are. I agree with previous answers, these are not of biological origin. I agree that the right arrow might point to something like a quartz clast, but the fracturing (almost parallel fractures) doesn't resemble the fracture patterns you would usually find in quartz clasts as quartz doesn't have any cleveages.
I would try posting a picture of normal polarized and one with crossed nichols. This would give others a better chance to give the right answer.
Other features that might be helpful: Does the mineral show pleochroism? How axial image (uniaxial, biaxial)? Is the mineral anisotrope or isotrope?
Best,
Eric
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We have found in the deep sea sediments in the Jurassic units in the Pontides of Northern Anatolia. The form that may be macrofossil that seen in the pictures. We are suspicious that this form could be a macro fossil (may be of ichthyosaurus). Is anyone have an idea what is this form fossils or another geological features?
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Hi,
The photo's are not clear enough to say anything. It seems there is a circular feature of a certain size, but if you are thinking this may be the vertebral column, then I cannot see any evidence for that. I cannot see any identifying features that would indicate bone.
I include some images that show what an icthyosaur fossil would normally look like.
Any more questions - feel free.
Best regards,
Remmert
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It has been seen along with possible Calpionellids and possible Saccocoma fragments.
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It resembles most likely bryozoan (or possibly some encrusting organisms...).
Best
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They have been seen along possible calpionellids
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First of all check whether these could be echinodermal pieces! Each echinodermal piece behaves like a single crystal and turns out black in one goal with cross-polars on when rotating the microscope stage. Because a single Saccocomid animal is made of numerous pieces you should have a lot of them in a single thin section, not few of them.
Obviously your material does not comprise any calpionellid!
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Hi people, i am looking for the following article: Abbink, O. A. (1998). Palynological Investigations in the Jurassic of the North Sea Region:(met Een Samenvatting in Het Nederlands): Proefshift Ter Verkrijging Van de Graad Van Doctor Aan de Universiteit Utrecht (...). Universiteit Utrecht, Faculteit Biologie. I can't get it anywhere. If anyone has a copy I would really appreciate it.
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Thanks Wolfram, I already tried to get in touch with them.
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We are working on belemnite jaws and this lead to the question to size limits in belemnite body size. The largest genus is undoubtedly Megateuthis from the Middle Jurassic.
The largest published record of a rostrum is around 500 mm in length to our knowledge.
In our collection, there is a phragmocone fragment where the largest septum has a diameter of over 130 mm.
However, there are certainly larger rostra and I wonder is one of you knows about much larger ones. A fossil collector owns a rostrum that is about 600 mm long, but I could imagine that this is not the limit yet.
I look for photos of larger rostra and phragmocones to get an idea of the upper size limit.
Thanks for your contributions!
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We only published figures of the type material of Volgobelus colossicus (Rogov, Bizikov 2006: http://mmtk.ginras.ru/pdf/Rogov,Bizikov,2006_Belemnoteuthis.pdf ), while this specimen is a recent finding by palaeontologist amateur
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The Jurassic shallow water fauna in Eurasia and Tethys is similar to fauna from western coast of North America. The migration is explained by two concepts:
Spanish Corridor – narrow seaway connecting Europe and western coast of North America
Panthalassa steppingstones – terranes located between eastern Asia and western coast of North America
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As far as I remember, there is no actual geological/paleontological evidence for the Hispanic corridor - it's just based on faunal similarity. And as Sylvain wrote, there is exchange across the present-day Pacific Ocean, so why not across Panthalassa back in the Jurassic?
Cheers, Steffen
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Superficially the reconstruction looks great. However, a moderate issue concerns the fitting of the blocks off Australia. In the published recon (Fig.3a-c), the Lhasa is placed flush against Australia's present-day shoreline - submarine features such as the Exmouth Plateau and the rest of the shelf, which is rather wide) are not accommodated. However, they cannot be ignored. Additionally, the last phase of rifting in the region (Jurassic, ?Middle to Late) had blocks departing from there so there must have been additional material separating the modern day Australian land-sea boundary from the Cimmerian fragments. This flaw is not restricted to the published study and has in fact been repeated in many recent Gondwana models. The topic is important, but this important issue is either being overlooked or ignored. In future publications this definitely needs to be addressed. Regards, Jason Ali (Hong Kong)
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Dear Hanbiao Xian. Thanks for getting back to me. The NW Australian shelf needs to be accommodated in all models to at least the start of the Paleozoic. The crust here has not been added to Australia during that time. To help you, I suggest you check out the recons shown in the latter part of: Palaeomagnetic re-investigation of Early Permian rift basalts from the Baoshan Block, SW China: constraints on the site-of-origin of the Gondwana-derived eastern Cimmerian terranes
JR Ali, HMC Cheung, JC Aitchison, YD Sun (2013) Geophysical Journal International 193 (5), 650-663. If you want, I could pass on the Coreldraw stencil. Robert Hall also give a lot of thought to this sub-region so you should consult some of his post 2010 papers.
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Corals and floral traces?
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The first figure is the coral Montlivaltia (Coelenterata) while the second is an impression of pinnate leaf of angiosperm.
Obianuju P. Umeji
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I found this ammonite in the Oxfordian Ammonitico Rosso from the Balearic Islands, Spain.
I would like to know the genus and the species if possible. I'm doubting between Phylloceras and Trimarginites.
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Triassic - Jurassic boundary
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Dear Ryan Shell, the foto4. The phytoplancton an Odontochitina operculata (O. Wetzel 1933a) Deflandre et Cookson 1955. Hungarian Age: Cretaceous, Senonian, Late Campanian; Williams et al. 1998 Age: Senonian; Williams et al. 1993: Hauterivian-Early Maastrichtian (117-73 Ma). Best regards, Mária.
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Following up with the previous questions, I found these specimens in the Oxfordian Ammonitico Rossos facies from the Balearic Islands, Spain. I would like to get some help identifying the genus and species of these 3 specimens.
I suspect that the second specimen, the one with primary and secondary ribs, could be a Taramelliceras.
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From the sample specimen that I saw like Belemnite for photo 1 & 3 for number 2 is ammonite, to determine the species of ammonite we need to note the shape of the suture on the wall in the form of Ceratite or goniatite.
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I need help identifying this ammonite species. It was found in the Oxfordian Ammonitico Rosso facies from the Balearic Islands, Spain.
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I am not an expert of Oxfordian ammonites, but according to the subcircular section in the very internal towers, then oval and finally subrectangular to subquadratic elevattion , I guess it belongs to Peltoceratoides, probably it's
( Gregoryceras pervinquieri (Spath,1913) )
Good luck
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Hi, nice meeting and talking to you in Quebec. I cannot find your e-mail address anywhere so I try here. Your new generic name for D. habilis? I can't remember it. What is it? and could you also provide me with a reference?
I am finishing a very big MS with a revision of the Jurassic stratigraphy of East Greenland and D. habichi occurs scattered in the paper. It would be useful with a more up-to-date name.
Cheers
Finn
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It is thought that A. afarensis was ancestral to both the genus Australopithecus and the genus Homo.
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Will the concept of science-fiction genetic experiments to recreate the long-extinct dinosaur species used in the plot of the film "Jurassic Park" ever be possible?
The plot of the film "Jurassic Park" directed by Steven Spielberg is based on a simple, but currently unrealistic concept of laboratory testing of the reproduction of long-extinct dinosaur species.
The collected genetic material of dinosaurs from the blood of a mosquito sunken for millions of years in amber is the main material on the basis of which extinct dinosaur species are recreated.
The genetic material obtained in this way introduced into the germ cell of modern reptiles in the film gives the possibility of reproduction of extinct reptile species.
This idea is based on modern research and genetic experiments carried out in laboratories, whose aim is to create, for example, new crop varieties or produce drugs for specific diseases.
However, the reproduction of long-extinct species such as dinosaurs is still not possible because the genetic material undergoes deep fragmentation over millions of years.
The genetic chain of chromosomes breaks down into very short fragments. So short that there is no information on how to assemble them into whole chromosomes and the lack of enzymes that would be able to fragment these fragmented dinosaur DNA pieces into whole chromosomes.
But the technology of genetic research is developing. The whole genomes of various species of animals, plants and other life forms are studied. The knowledge base of genotypes and related species is successively growing in the Big Data resources created for this purpose.
Therefore, the question arises: Will the fantastic research concept applied in the plot of the film "Jurassic Park" ever be possible? Will it be possible to recreate long-extinct animal and plant species with the help of subsequent generations of research in the field of genetics in the future?
Will it be possible to create a real Jurassic Park in the future, within which dinosaurs will run among the vegetation composed, among others, of flowering and woody ferns, horsetail and ferns, or the restoration of the ecosystem from millions of years ago?
Or maybe a man should not even try this type of other than present ecosystems to play?
Is this also a matter of ethics? Is it not threatening modern ecosystems to restore ecosystems over millions of years, ie consisting of many long-extinct species of plants and animals?
Please, answer, comments. I invite you to the discussion.
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Hi there!
That's actually a very nice question!
First of all, I am not the best person to answer this, but I would suggest you the book "How to clone a Mammoth" by Beth Saphiro. This is a great reading that answers a lot of your questions!
The main issue with the idea of using fossils to obtain genetic material is that "fossils" usually have organic parts substituted by minerals (processes called 'permineralization' and 'recrystallization'). Therefore you cannot extract DNA from these fossils because everything was substituted by minerals. It is also true that recent studies seem to have found traces of soft tissues in extremely well preserved fossils, but this is still extremely far from allowing to obtain the genome of dinosaurs (if you are interested in this, check the works of Mary Higby Schweitzer --> https://en.wikipedia.org/wiki/Mary_Higby_Schweitzer#cite_note-18).
However, the movie played it quite smartly on this topic, suggesting that the blood was actually encased in the amber, therefore not really fossilized. Nonetheless, in the book cited above, they explain how they tried to obtain even the DNA of insects from amber (I seem to recall they were working on bees?) but always failed. Again, a team of researchers managed to found "emoglobin-derived porphyrins" in a mosquito encased in amber ( ), but this is still far from Jurassic Park, still.
What you can extract DNA from, is frozen material. That's how they managed to obtain the full genome of the wholly mammoth (in 2015) from frozen specimens unearthed from the ice of Siberia. And yes, there is already who is thinking of using it to inseminate elephants in order to be able to have their "Pleistocene Park" (I now it's in Siberia but I do not remember additional information, again, check the book!).
This obviously generated a lot of discussion on the idea of how ethical it would be to use elephants to breed mammoth.
Sorry for the long answer, but I truly find this topic extremely exciting!
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Unknown stratigraphic position, found in scree deposits in western Greece. Jurassic up to Eocene carbonate successions is the source for the scree. Conglomerate or breccious limestones are reffered and have been observed only in the middle-late Cretaceous interval, which is not in accordance with early-Jurassic extinct order of the Spiriferida. What else can it be? Expert opinions?
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Definatelly a clypeasteroid echinoid. Well preserved and not at all dissolved cross-section of Clypeaster test.
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Dear Researchers,
I have collected some Abor volcanic rocks from the Siang Valley, NE India, interestingly the volcanic rocks have shown the Upper Jurassic to Lower Cretaceous age which is different than the previous literature. Is it possible that the Abor Volcanic was emplaced during Indian subcontinent breakup event from Gondwana?
Regards
Upendra
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Crustal blocks have been departing Gondwana for a very long period - " emplace(d) during the time of Gondwana breakup" is a very vague statement. If India is thought of as the "core" of Gondwana (the label is, I believe, derived from an Indian group of people/culture), breakup events have happened through the Paleozoic (mid-Early Paleozoic) through Mesozoic (end-Cretaceous - Seychelles). What specifically do you mean?
Regards Jason
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Problem is slove
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What was the original carbonate mineralogy, LMC or HMC/Aragonite (during the Jurassic it could've been either)?
What is the current mineralogy? If it's different, then your rocks have undergone neomorphism (near certainty that they did) and your d18O values reflect the temperature and water d18O during neomorphism.
Then ask yourself the following questions:
1.) What was the temperature of neomorphism/formation?
2.) What were the potential fluid sources?
3.) Was there a meteoric fluid source?
4.) What were possible d18O values of your fluids?
Then with that data, plug it into calcite-water fractionation equation e.g. Friedman and O'Neil (1977) and see if you get realistic values.
Examples:
Seawater with a d18O of 0 per mil VSMOW at 25 oC produces a calcite with -2.45 per mil VPDB.
Seawater with a d18O of -2 per mil VSMOW at 25 oC produces a calcite with -4.39 per mil VPDB. (The upper end of your values)
Seawater with a d18O of -2 per mil VSMOW at 45 oC produces a calcite with -8.08 per mil VPDB. (The lower end of your values)
Now it's up to you to figure out if those are realistic temperatures or fluid d18O based on other data. I agree with Xue-Ming Yang that even if meteoric waters interacted with your rocks, the d13C may still reflect the original carbonate values.
To see an example of how to do this you can check out my publication:
And the calcite-water fractionation equation is below:
Good luck!
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We are looking for someone to help us determining Callovian-Oxfordian (and possibly Kimmeridgian) benthic foraminifera in order to date carbonate platform successions.
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Raphaeel:
Kindly contact Dr. Kemal Tasli at : ktasli@mersin.edu.tr for expert advice.
Best
Syed
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The propose of the electrical resistivity tomography sections is mapping bedrock of a free aquifer in a depth of ~50m. The basin with an area of ~ 65 km² is located in an outcropping area of Guarani Aquifer System, formed by eolian-sandstones from the Jurassic Period (Botucatu Formation) and fluvio-eolians from the Triassic Period (Piramboia Formation). Therefore, it is covered by Cenozoic sediments, with variable thickness in tens of meters.
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Well,
The attached article explains a geophysical study performed east of Rutba town due to vertical electrical sounding in a net of forty points between Dhalaa and Dhabaa valleys. Geophysical electrical model applicated using Winsev 6 program to determine the geo-electrical layers.
https://www.researchgate.net/publication/303933182_GeoElectrical_ Investigation_of_Mullusi_Aquifer_Rutba_Iraq
Sincerely
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It come from dolomitic limestone from South-East of France dated from Kimmeridgian (Late Jurassic) following the geological map. This specimen looks like to an Oppeliidae such as Streblites??
What is your opinion? And I know, it 's very poorly preserved, but it is the best specimen!
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Thanks a lot Luc,
It's a pleasure to have some news of you. Yes I know, It's very damage because this surface (probably a condensed surface) is plenty of belemnites and ammonites, even large specimen of 20 cm. Unfortunately the dolomitization and the bad preservation give us bad material... You which work on the area, did you have some publication on Upper Jurassic of the area of Saint-Vallier du Thiez?
Thanks a lot,
Cheers
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I need to paleogeographical maps of Middle Jurassic from world and Asia.
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this sample represents a Jurassic carbonate sediment (from NE Algeria). It is followed by dolomitized limestone . Thank's in advance.
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There is no single process that can be called "dedolomitization". The dolomite may be dissolved with calcite cement filling the pored or may be replaced by calcite (calcitized). It is better to describe these than to use an imprecise and basically undefined word. Your images ar unfortunately insufficiently detailed to determine the process tha has occuerred. The advice of other correspondents recarding CL and staining is worth following up.
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I look for this article, but is so old for be uploaded: E. Bölau. 1954. The first finds of dinosaurian skeletal remains in the Rhaetic-Liassic of N.W. Scania. Geologiska Föreningens i Stockholm Förhandlingar 76(3):501-502
The questions are: the collected are exposed? any affiliation? any new study?
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Antonio:
You may see this publication and the references therein for possible clues to your question:
Best
Syed
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These diffractograms represents a Jurassic dolomite sediment (from NE Algeria). . Thank's in advance.
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in order to index all the peaks
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This object was found in a ploughed field near Yeovilton in Somerset, England. The underlying rocks are fossiliferous limestones and mudstones of the Lias Group, Lower Jurassic. Fossils found in the ploughed field include ammonites and bivalves, which are typical of shallow marine seas. However, this object does not look like a fossil (e.g. interior cast of an ammonite) in my view, but rather like a piece of sandy clay that has been shaped and smoothed by hand while wet and then baked in the sun. As I did not collect the object and have not visited the locality, I cannot say what other geological or archaeological context or clues might have been present. I just wondered if anyone recognizes this "cashew-nut" look-alike as either a spurious geological curiosity, or as a possible human-made implement (scraper?) or decorative archaeological object?
Dave
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D.M. Evans
Observando el ejemplar ilustrado considero que se trata de la camara de un  Nautiloideo, como lo ilustro en la siguiente imagen.
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The enigmatic structure is indicated by the yellow arrows (look at the photo). The scale bar is in centimetres. I'm not sure what it could be. It was found in carbonate sediments of Upper Jurassic from the Carpathian Foreland of Southern Poland. Thanks!
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It looks like Gastropods recorded within carbonate shallow marine environments (lagoonal or back-reef )
We can also see some fenestrae/birdseyes !!! stromatactis!!! attesting of arerial exposition!!!!
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Any one who had worked on Early Jurassic Palynology/ Need to Identify some polymorphs species.
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Dear Nasar,
May I see the photos?
Best wishes
Anna
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I am trying to use palynomorphs instead of biomarkers for correlation. Any one having expertise and suggestions.
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Yes as palynomorphs faced some physiochemical changes during migration and even their size is also lager in some cases than reservoir pores. Thus biomarkers usage will be more genuine for oil source rock correlation.
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I've attached a pdf with 4 ostracod photos.  The sample comes from an "ostracod ironstone", thought to be Early Paleozoic, Mackenzie Mountains, western Northwest Territories Canada. The nesting is the curiosity. Thanks.
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Terry,
In the most striking example of nesting I notice that there there appears to be fine clastic sediment between each molt stage. The main set of nested valves in the previous set may be in opposite orientation to the largest one. Also, if you look at all of the material, most of it is not nested. It suggests to me that sometimes the valves are moved around a bit and they, occasionally, just fit together.
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Because i think that i have sand dikes injected in a sandstone, but i can observe or identificate the unit source for where came from
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Thanks for the answer Mr. Dill.
I've been working with fluvial deposits and saw several injectites like that case in the picture. In one thick sandstone layer (mayor channel) saw a few sand dikes injected but i can´t find the source of the material. I inferred that the layer suffers liquefaction and fluidization and the injection happens in the same layer. Is an assumption, but i´m not sure.
(Apologies for my english)
Regards
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what are their responses to the environmental changes
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In the year 1990 I could find an interesting fossil object (see fotos attached) in the Solnhofen Formation ("Solnhofener Plattenkalke", Malm Zeta 2b) at the locality "Blumenberg" near Eichstätt (Bavaria, South Germany). I don't know to what animal, perhaps to a cephalopod (? nautiloid or ammonoid jaw fragment), this fossil remain belongs to!
The scale/dimension of the fossil object is the following: 4,5 x 2,7 centimeter (max. length x max. wide); the convex surface shows little "points" and "fold structures".
Do you have an idea, to what animal this Upper Jurassic fossil belongs to? Please give me informations and/or fotos for comparisons!
Thanks very much;
Volker
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Hi, Volker,
the visible morphology does not support the suggestion of a coprolite well. The "drying lines" or dents would not be expected in a coprolite. Drying dents require at least a coating such as a cuticula or soft shell, under which the drying would occur, or it could be a soft carapace that shows folding. If it were a coprolite, drying or concentration of the mass would appear more or less uniform. The surface would be more or less uniform granular, unless some undigested bodily ingestations are within.
Also, the punctiform indentations do not fit to a coprolite. Certainly, it is difficult to ascertain. To me, a possible explanation is a crustacean shell, e.g. an ostracode shell or that of a bivalved crustacean. It may have been shortly after moulting, thus still flexible and soft.
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We find some fossil plant remains in Late Jurassic rocks.
Can anyone identify this remains?
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Alejandro:
Provide some basic data about the host rock yielding these fossils and other fossil remains in a litholog, if any. If the Late Jurassic rocks are shallow marine deposits you may expect terrestrially derived silicified / petrified wood fossils in high energy coarse grained marine Sandstones. You need to examine thin sections of these fossils to determine taxonomic affiliations.
Best
Syed
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This specimen found in the Badamu formation.
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I fail to see the spiral striae or the lateral furrows typical for Strigoceras on these photographs.
I am wondering if it could be Oxycerites species but those with stronger ribs are usually later than Bajocian. To my kowledge the Badamu Formation only goes up to middle Bajocian near Kerman (is this correct?) which makes it even less likely to be an Oxycerites.
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Can anyone help me to determine ammonites which I found in Bathonian to Callovian age?
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Consult the Thesis and works of Prof. Guillermo Meléndez
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When I read some articles, I found the time was not consistent to the geological time scale. For example, In the Article Archaefructaceae, a new basal angiosperm family ( Sun G, 2002), the fossil was inferred 124.6 mya, and arttributed to upper Jurassic of China. I checked the geological time scale, the Jurassic was between 201.3 mya and 152.1 mya and Cretaceous began 145 mya. How to explain this?
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In the article by Sun (2002), they had a small note stating the following:
(9) The age of the Yixian Formation of western Liaoning, China, is uncertain. We allow for a range from 145 to 125 million years, which corresponds with the Upper Jurassic to Lower Cretaceous (12, 31, 38–45).
Therefore, at that time, they didn't know whether it was Late Jurassic or Early Cretaceous in age. Be aware that since then, there has been new radiometric datings for the Yixian Formation in China showing that it was actually Early Cretaceous in age:
There is a review of all radiometric datings for this Formation in Wu et al. (2013), Palaeo3 and even an astronomical calibration so it appears that this Formation is now very well dated. 
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From this formation Come the Fossils of Cryolophosaurus and Glacialisaurus
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Thanks
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 The enclosed photographs are from Upper Jurassic - Lower Cretaceous fluvial succession of Gondwana. I am of the opinion of their origin through biogenic activities, however, not very sure. The preservation of the structures is in light to dark gray clayey horizons having abundant leaf impressions of Pteridophytic to Gymnospermus remains. The clay units occur as interbedded horizons with siltstone or, lenicular/poketed occurrence in medium grained sandstone
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Thanks for comments, interesting, approach you shortly.
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If it´s possible omit the related to Cryolophosaurus and Glacialisaurus
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Hi Antonio,
This article is not cited by Smith et al. (2007) for obvious reasons: Carpenter, F.M. 1969. Fossil insects from Antarctica. Psyche 76: 418-425 (Toarcian dragonfly Caraphlebia antarctica)
Cheers,
Mike
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Jurassic deposits of the Siberia and NE Russia are characterized by numerous glendonite occurences, especially widely distributed in Upper Pliensbachian and Bajocian-Bathonian. Did anybody know any information about the coeval glendonite occurrences in Northern America? I know only two briefly mentioned records of "stellate nodules" in the Kimmeridgian of Northern Yukon and Mid Volgian of Prince Patrick Island 
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I don't know about North America, but glendonites have recently been found in upper Pliensbachian sediments in Northern Germany from the Shandelah core. See Teichert, B.M.A., Luppold, F.W. (2013) Glendonites from an Early Jurassic methane seep – Climate or methane indicators? Palaeogeography, Palaeoclimatology, Palaeoecology, 390, 81-93.
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Can anyone send or recommend me a good paper about Upper Jurassic Carbonate Geologic settings in Western Desert, Egypt??
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Dear Aser
you can check the link below which deals with Tassy et al. (2015) entitled Egyptian Tethyan margin in the Mesozoic: Evolution of a mixed carbonate-siliciclastic shelf edge (from Western Desert to Sinai).
Abdou et al. (2009) have been documented subsurface Jurassic sediments of Western Desert (see link below0
Regards
Massih 
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This fossil Himenofitales fern was collected several years ago by R. Rojas and myself from a Jurassic pre mid-Oxfordian exposure of the San Cayetano Formation in western Cuba. Any suggestion as to species or genera or distribution in time and space?
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Another detail of the same taxon.
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Dear colleagues!
Can anybody help me with one biological/paleobiological question? Recent Nautilida, as well as many ancient nautiloids, have a cicatrix on their embryonic shell. During formation of the embryonic shell the area of cicatrix initially forms from organic material and later became calcified. Very likely, the shell with cicatrix was the basal type of cephalopod embryonic shell, the second type with protoconch could have appeared later. Monoplacophora is considered as cephalopod ancestor, but I have never seen cicatrix in their shells. Do you know any examples of cicatrix in non-cephalopod mollusks, especially in fossil or modern Monoplacophora?
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The photos of nautiloid cicatrix are from my own collection and from the article R.Chirat, S. Von Boletzky (2003) Morphogenetic significance of the conchal furrow in nautiloids: evidence from early embryonic shell development of Jurassic Nautilida
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Dear Dr.Bulot, dear Dr.Fuchs
Thank you very much for your help!
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I may suggest you to contact Kevin Page: kevin.page@plymouth.ac.uk 
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This specimn found in the Badamu Formation.
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Hello Tayyeb,
I'm sorry to say that in my opinion, an identification based solely on the view given in this photo is nigh on impossible. For the positive identification of a species one needs  to see the shell or mold with ribs and whorls, and also views of the external side and the mouth aperture, or at least the molds thereof. Am I correct in assuming that the Badamu Formation is of lower Bajocian age?
I have however just found something here which may be of help to you:
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Working at the southern Central Andes we have found some interesting features. In the hinge zone of a broad (ca. 6 km) basement-cored anticline there are sub-vertical clastic dikes of breccia cutting the sequence. The basement is composed by Paleozoic metamorphic rocks and granites and is cropping out several km away from the dikes outcrop. It is covered by Jurassic volcanics of the syn-rift stage of the Neuquén basin. The dikes have between 1 and 3 meters wide and are not oriented in none particular strike. The breccia is composed by basement and syn-rift volcanics angular clasts and boulders ranging from 1 cm up to 50 cm. We are working with the structural data obtained from field work and are interested in any reference we can use to better understand their genesis. The timing of the intrusion is not clearly related with folding, it could be more related with a prior extensional stage in the region...
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I also just remembered of this Clastic Detritus blog:
No idea if it has been published a bit more
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Who worked on Early Toarcian OAE  based on  ammonites and nanofossils ?
Is there an article on this topic?
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An interesting but very old paper about nannofossils and ammonites during italian toarcian:
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We analyzed 8 samples of alterated jurassic basalts. Analysis results of major oxides are attached to this question as a word document. 
What is the reason of high K2O and low total Fe2O3?
Thanks.
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Dear Mr. Dadpoor,
First and foremost it is important that you can trust in your analytical devices and methods applied. I do not know of what type of samples (e.g. powdered, broken) you avail yourself. Thin sections may be on option but in the majority of cases you have to resort to methods like XRD, IR, and CEC, due to the particle size of the minerals newly formed  during alteration. For field and first-hand information PIMA (SWIR) is of value to get an overview of the alteration minerals present in the volcanic rock. This works for genetic and applied issues alike. You must test your chemical data in case of alteration, particularly in such fine-grained rocks (I did not see a specimen so it is only an assumption). For further reading I can recommend the paper below which I can also "send privately" upon request.
Methods and discussion are published in the following papers
DILL, H.G., SIEGFANZ, G. and MARCHIG, V. (1994) Mineralogy and chemistry of metalliferous muds forming the topstratum of massive sulfide-metalliferous sediment sequence from East Pacific Rise 18°S: Its origin and implications concerning the formation of ochrous sediments in Cyprus-type deposits.- Marine Georesources and Geotechnology, 12, 159-180. (Fe smectite and Fe oxide hydrates mainly)
DILL, H.G., FUESSL, M. and BOTZ, R. (2007) Mineralogy and (economic) geology of zeolite-carbonate mineralization in basic igneous rocks of the Troodos Complex, Cyprus.-Neues Jahrbuch für Mineralogie Abhandlungen, 183: 251-268. (carbonate, zeolite, clay)
DILL, H.G., DOHRMANN, R. and KAUFHOLD, S. (2011) Disseminated and faultbound autohydrothermal ferroan saponite in Late Paleozoic andesites of the Saar-Nahe Basin, SW Germany: Implications for the economic geology of intermediate (sub)volcanic rocks.- Applied Clay Science, 51: 226-240. (clay minerals)
DILL, H.G., TECHMER, A., BOTZ, R., DOHRMANN, R. and KAUFHOLD, S. (2012) Hypogene and supergene alteration of the zeolite-bearing pyroclastic
deposits at Tell Rimah, Jordan, and rift-related processes along the Dead-Sea-Transform Fault System during the Quaternary.- Journal of Volcanology
and Geothermal Research, 239-240: 49-68. (zeolite, carbonate, clay minerals)
K can be accommodated in the lattice of micaceous phyllosilcates but als appear in zeolites.
I think for a more focused discussion you need to disclose the type of sample to the people interested in that issue. Then I am convinced that a solution to your problem is not anything out of the ordinary and you will even find somebody providing technical assistance.
Best regards and good luck
Harald G. Dill
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It has been shown that different populations of the same plant species can produce longer or shorter n-alkanes for their wax in response to water stress and/or temperature. I would like to know if one specimen at one site can modulate the chain-length of its n-alkane in response to seasonal environmental variation. It is for Paleoclimatic application (Lower Jurassic).
Regards
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Thank you for this reply
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I am looking for the identification and naming strategy for the pollen and spores pertaining to the Jurassic system. Can anyone help me and guide me for any literature and/or catalog available in this regard. Thank you all
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If you are still looking for literature and catalogues for Jurassic palynomorphs then you may want to visit the John Williams Index of Palaeopalynology at the Natural History Museum, London. This is a cross-referenced database of all published taxa and publications and is very good for the Jurassic (I use it all of the time for the same purpose). There is also a personal library with all of the publications to hand. Feel free to contact me to find out more or to organise a visit