Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Oive Tinn"'
Publikováno v:
Estonian Journal of Earth Sciences, Vol 70, Iss 1, Pp 51-69 (2021)
The Late Ordovician Baltic Palaeobasin (BPB) offered a favourable environment for a diverse and abundant ostracod fauna to thrive across the basin. A short period of unstable environmental conditions at the end of the Ordovician, the Hirnantian glaci
Externí odkaz:
https://doaj.org/article/09a7f29569794d4781c9b1c89b1867f3
Publikováno v:
Estonian Journal of Earth Sciences, Vol 69, Iss 4, Pp 233-247 (2020)
Ostracods of the Ordovician and Silurian transition interval in the JÅ«rmala section, Latvia, were studied. The diverse pre-Hirnantian ostracod assemblage is replaced by the Harpabollia harparum association that has been recorded across the Baltosc
Externí odkaz:
https://doaj.org/article/3896af70e2b24c9b9067d9aa2c1b0083
Publikováno v:
Estonian Journal of Earth Sciences, Vol 69, Iss 4, Pp 223-232 (2020)
On the basis of detailed SEM-EDS study and computer tomography scanning, the single specimen of the enigmatic Martsaphyton moxi from the Aseri Stage (Darriwilian; Middle Ordovician) of Estonia, was identified as a member of the phylum Cnidaria and su
Externí odkaz:
https://doaj.org/article/6c07a51777f141b281d452131c2425f6
Publikováno v:
Estonian Journal of Earth Sciences, Vol 69, Iss 4, Pp 214-222 (2020)
The Middle Darriwilian Isotopic Carbon Excursion (MDICE) is a global isotopic event described in sections from different palaeocontinents. Here we present new stable carbon isotopic data from carbonates of ten sections in different parts of the Balto
Externí odkaz:
https://doaj.org/article/abdc2d6f3cc04a139e3ace0261b5318d
Publikováno v:
Estonian Journal of Earth Sciences, Vol 68, Iss 1, Pp 1-14 (2019)
A metre-scale thick siltstone–sandstone lobe is described within the Dapingian outer ramp argillaceous limestone facies of the Baltoscandian palaeobasin. This bed is referred to as the Volkhov Oil Collector in previous studies due to its hydrocarbo
Externí odkaz:
https://doaj.org/article/0660f57bf574402d96ee41d6939c349d
Publikováno v:
Estonian Journal of Earth Sciences, Vol 65, Iss 2, Pp 105-114 (2016)
The Kalana quarry in central Estonia is known for its exceptionally well-preserved non-calcified algal and other fossils. The interval with the fossil Konservat Lagerstätte in the Kalana section has previously been tentatively dated as early Aeronia
Externí odkaz:
https://doaj.org/article/291a2bde1729439e826cfa6f272960cb
Autor:
Maris Rattas, Volli Kalm, Kersti Kihno, Elsbet Liivrand, Oive Tinn, Kati Tänavsuu-Milkeviciene, Maire Sakson
Publikováno v:
Estonian Journal of Earth Sciences, Vol 59, Iss 2, Pp 125-140 (2010)
The information obtained from a 21 m thick open-pit section of silty-clayey sediments in the Arumetsa bedrock valley, southwestern Estonia, revealed that lacustrine to glaciolacustrine sedimentation at the site started prior to 151 ka ago and lasted
Externí odkaz:
https://doaj.org/article/3cbcea4576c04093a362dba20ae57700
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 307:41-50
Publikováno v:
Lethaia. 55:1-13
Publikováno v:
Palaeoworld.