Microfossils from the Lower and Middle Miocene of the brown-coal exploration well Lübtheen 46/84 (SW Mecklenburg)

1992 ◽  
Vol 1992 (3) ◽  
pp. 150-170 ◽  
Author(s):  
Jutta Rusbült ◽  
Christoph Strauß ◽  
Jürgen Haupt
2016 ◽  
Vol 78 (6) ◽  
Author(s):  
Yulfi Zetra ◽  
Imam B. Sosrowidjojo ◽  
R. Y. Perry Burhan

A section of the Sangatta coalfield in the Balikpapan formation located in Kutai Basin, East Borneo, Indonesia, is the Inul area, located North of Pinang Dome. This section of the coalmine has coals with low calories (ca. 4379 cal/g), which is why they cannot be used optimally yet. The reasons of using low calorie coals are besides from being used as a mixing ingredient for the blending process of high calorie coals, they are also used to diversify the coals through the process of coal liquefaction (coal to liquid). In order for the coal liquefaction to be processed correctly, there needs to be a study on the geochemistry organics through coal biomarker analysis, particularly on the hydrocarbon aromatic fractions, so that the origins of the coal organic compounds could be known. Biomarker analysis on the aromatic hydrocarbon fraction shows the existence of naphthalene compound groups with sesquiterpenoids skeleton, phenanthrene with diterpenoids, sesterpenoids skeleton and triterpenoids aromatic pentacyclic. The existence of cadalene compound, triterpene pentacyclic monoaromatic, -triaromatic, -tetraaromatic, -pentaaromatic and triterpenoid C-ring cleaved hydrocarbon with oleanane, ursane and lupane skeletons indicated that the source of coal organic compounds were derived from b-amyrin which were produced by Angiospermae plants. The coal biomarkers distribution, particularly the high abundance of triterpenoid pentacyclic triaromatic compound, confirmed the low maturity of the coals which is predicted to profit from the process of liquefaction due to the high contents of their aromatic fractions.


1986 ◽  
Vol 60 (4) ◽  
pp. 968-970 ◽  
Author(s):  
Jonathan J. Becker

The genus Ardea includes all living species of large herons. Brodkorb (1963) listed five fossil species of Ardea, and only one fossil species has since been described. Of these six, only two are unquestionably members of the genus Ardea. Ardea brunhuberi von Ammon, 1918, from the Upper Miocene Brown Coal Formation, Württemburg, Germany, was moved by Brodkorb (1980) to the Phalacrocoracidae as Phalacrocorax brunhuberi. Brodkorb (1980) considered A. lignitum Giebel, 1860, from the Sarmatian Brown Coal of Rippersroda, Thuringia, Germany, to be a large owl in the genus Bubo. Olson (1985) similarly regards A. perplexa from the Astaracian of Sansan, France, to be a large owl, possibly in the genus Bubo. The type of Ardea aureliensis Milne-Edwards, 1871, from the Oreleanian of Suevres, France, has never been illustrated or restudied and its affinities need to be confirmed (Olson, 1985). The valid fossil species are Ardea polkensis Brodkorb, 1955, from the late Hemphillian Bone Valley Mining District, Florida, and A. howardae Brodkorb, 1980, from the Plio/Pleistocene Shungura Formation, Omo Basin, Ethiopia. A large species of Ardea is also known from the late Clarendonian Love Bone Bed local fauna, Florida, but is based on material too fragmentary for specific identification (Becker, 1985). This note reports the earliest certain occurrence of Ardea now known.


1999 ◽  
Vol 154 (4) ◽  
pp. 339-352 ◽  
Author(s):  
Andreas Lücke ◽  
Gerhard Helle ◽  
Gerhard H. Schleser ◽  
Isabel Figueiral ◽  
Volker Mosbrugger ◽  
...  

2016 ◽  
Vol 78 (7) ◽  
Author(s):  
Yulfi Zetra ◽  
Imam B. Sosrowidjojo ◽  
R. Y. Perry Burhan

Organic geochemical studies on brown coal (lignite) located in Inul area were carried out, an area that is located in Sangatta coal mines, East Borneo, which is a part of the Balikpapan formation, aged as old as Middle Miocene to Late Miocene. Aliphatic hydrocarbon biomarker compounds which were identified by using the GC-MS analysis showed a presence of n-alkane (n-C12-n-C36) with bimodal distribution, which described the sources of organic compounds that originated from two different sources. These sources of organic compounds are phytoplankton, zooplankton and higher plants terrestrial. The Pr/Ph ratio of 1.3, the dominance of C31-homohopane and a high ratio of Tm/Ts indicated that the process of peat depositions took place in an oxic environment.  The existence of hopanoid contents showed that there were dominant activities of microbes and biolipids organic compounds such as bb-hopane and hop-17(21)-ene inside the samples of olean-12-ene and a-cadinene, which inidicated that they are organic compounds that came from higher plants such as Angiosperm and immature coals. The existence of 24-ethylcholestene and 5b-cholest-24-ene found in the coal samples, which are categorised as steranes, also indicated a low level of carbonization from the coal itself. 


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