The quality of coal has been analyzed basing on the data from geological exploration and chemical – geological analyses of coal carried out on the samples obtained from the boreholes and mining pits. The operated coal seams indexed as 382 and 385/2 reveals the changeable morphology due to the thickness of carbon shoals and stent intergrowths. The other parameters, such as the ash content or the calorific value are strongly linked with the non-coal rock interlayers, which presence causes the decrease in the calorific value and increase in the amount of after-burning ash. These parameters are less dependable on the sedimentation environment of the coal formation material. The content of total sulfur in the analyzed seams does not show any link with the values of the parameters analyzed before. The total sulfur is made up from sulphide gathered in coal and sulphates deriving from the decomposition of plants and supplied by deposit waters in different phases of coal seam formation. The obtained results could be useful in the reconnaissance of the prospective seams lying below the currently exploited ones (e.g. 389) and the seams in the neighboring areas.

The study included bituminous coal seams (30 samples coal from the Bogdanka and Chełm deposits)

of the Lublin Formation, the most coal-bearing strata in the best developed and recognized in

terms of mining parts of the Lublin Coal Basin in Poland. High phosphorus concentrations in coal of

the Lublin Formation were found (1375 g/Mg) as well as P2O5 in coal ash (2.267 wt%). The phosphorus

contents in coal and coal ash from the 385 and 391 coal seams in the area of the Lubelski Coal Bogdanka

Mine and in the area of its SE neighbor is the highest (max. 2.644 wt. % in coal and 6.055 wt. %

of P2O5 in coal ash). It has been shown that mineral matter effectively affects phosphorus contents

in coal and coal ash. At the same time, phosphate minerals (probably apatite and crandallite) present

in kaolinite aggregates of tonsteins contain the most of phosphorus and have the greatest impact on

the average P content in the 382, 385, 387, and 391. The secondary source of phosphorus in these

coal seams and main source of phosphorus in these coal deposits that do not contain mineral matter

of pyroclastic origin (378, 389, 394) may be clay minerals, which absorbed phosphorus compounds

derived from organic matter released during coalification. Phosphorus-rich ash from the combustion

of the Lublin Formation coal tend to be environmentally beneficial to the environment and also useful

for improving the soil quality. Due to the low degree of coalification and high content of phosphorus

in coal, this coals of little use for coking.

A sample of late Viséan limestone from the Włodawa IG-4 borehole, east of Lublin, Poland, yielded a piece of a tooth and a few hundred well-preserved scales comparable to those of “Ctenacanthus” costellatus Traquair, 1884 from Glencartholm, Scotland, UK. Most of the scales are typical compound body scales of the ctenacanthid type. Their crowns are composed of several separate odontodes whose distal ends are turned backwards and bases are characterised by concave undersides. In the material, there are also sparse scales with similar crowns but with flat or convex bulbous bases, as well as ornamented plates and single, star-like denticles, probably from the head region. The taxonomic status of “Ctenacanthus” costellatus was analysed and a new generic name for that species, viz. Glencartius gen. nov., is proposed.