Drzewica Formation

The Drzewica Formation between Gowarczów and Rozwady, forms sandstone complexes of +10 or so meters, usually uniformly formed, finely less often medium-grained, separated by Silt-sandstone blocks, sandstone-like places or Siltstones.{{cite journal |last1=Cieśla |first1=A. |title=Budowa geologiczna strefy wychodni liasu między Gowarczowem a Rozwadami |journal=Geological Quarterly |date=1979 |volume=23 |issue=2 |pages=381–394 |url=https://gq.pgi.gov.pl/article/view/9193/7744 |access-date=8 October 2021}} In these sediments there are worm tubules (Ichnofossils), Rhizoids and the remains of Charred plants, sometimes thin carbon inserts. This section on the area of Gowarczów-Rozwady wasn't completely covered, but connects the appearance of the Drzewica Formation strata with several coeval Boreholes: Gowarczów (GW-1 and GW-2), Kuraszków (KP-1 and KP-4), Sielec (A2), Adamów (Al), Kraszków (MG-2), Gielniów (GG-1) and in a few exposures (quarries) from the vicinity of Kraszków and Gielniów. On this region the most complete profile of this formation was obtained in the Sielec Borehole (A2), which was pierced by the geological structure of the outcrop zone, covering the middle and upper section of the Drzewica Formation with a thickness of 146.7 m. Locally, the thickness of this series is estimated at 175–180 m.

At the Late Pliensbachian (Margaritatus-Spinatum) several changes occur on the Polish Basin.{{cite journal |last1=Barth |first1=G. |last2=Pieńkowski |first2=G. |last3=Zimmermann |first3=J. |last4=Franz |first4=M. |last5=Kuhlmann |first5=G. |title=Palaeogeographical evolution of the Lower Jurassic: high-resolution biostratigraphy and sequence stratigraphy in the Central European Basin |journal=Geological Society, London, Special Publications |date=2018 |volume=469 |issue=1 |pages=341–369 |doi=10.1144/SP469.8 |bibcode=2018GSLSP.469..341B |s2cid=134043668 |url=https://www.researchgate.net/publication/322268601 |access-date=8 September 2021}} The last section, latest Raricostatum subzone, there were a series marine transgressive surfaces, linked with the called Pli1 transgressive phase, known thanks to molluscs and ooids, along with an increase of marine macrofauna and microfauna. A marine Ingression filled the Polish basin, depositing marine dark Clay, Mudstone and lenticular Heteroliths, that are abundant on the lower-Middle Pliensbachian Łobez Formation and Poland, where dark-grey marine Claystones appear on the Kaszewy 1 borehole. There was a visible shoreline retreat that ends on the beginning of the Late Pliensbachian Margaritatus Chronozone. After the Pli1, a series of local subordinate retrogradational stratal-pattern architectures indicate the transgressive phase of the sequence Pli2. Pli2 The transgressive phase led to a maximum flooding level at the middle Spinatum. That was known thanks to Ammonites found on an 85 m basin at NW Poland, on the Wolin IG-1 borehole.{{cite journal |last1=Kopik |first1=J. |title=Fauna osadów domeru Dembowska, J.Wolin IG 1. Profile Głębokich Otworów Wiertniczych |journal=Instytutu Geologicznego |date=1975 |volume=1 |issue=1 |pages=22, 53}} This transgression also impacted deposition, with 265 m sequences of Mudstones and sandstones in a syndepositional tectonic graben at the Wolin-Recław Zone.{{cite journal |last1=Dadlez |first1=R. |title=Stratigraphy of the Lias in Western Poland |journal=Prace Instytutu Geologicznego |date=1969 |volume=57 |issue=1 |pages=1–92 |url=https://gq.pgi.gov.pl/article/download/13274/11722 |access-date=8 October 2021}} After the maximum peak of the flooding basin it followed a regressive phase, characterized by progradational fluvio-deltaic sandstones, like the series of sandstones that recover the major tracksites of the Drzewica Formation, the Śmiłów Quarry Tracksite and the Wólka Karwicka Tracksite, both know from a regression nearshore/barrier lagoonal derived sandstone deposit. The Coeval deposits of Usedom and East Prignitz on Germany contain numerous Glendonites (Calcite pseudomorphs after Ikaite), what lends support to the possibility of a Late Pliensbachian cooling event and polar Glaciation at that time.{{cite journal |last1=Rogov |first1=M.A. |last2=Zakharov |first2=V. |title=Jurassic and Lower Cretaceous glendonite occurrences and their implication for Arctic paleoclimate reconstructions and stratigraphy |journal=Earth Science Frontiers |date=2010 |volume=17 |issue=17 |pages=345–346 |url=https://www.researchgate.net/publication/285506543 |access-date=8 October 2021}} Mostly of the authors, based on the current scientific quorum and the wide distribution of Glendonites in Upper Pliensbachian strata, tend to support a glacial-derived hypothesis.{{cite journal |last1=Ruhl |first1=M. |last2=Hesselbo |first2=S.P. |last3=Hinnov |first3=L. |last4=Jenkyns |first4=H. |last5=Xu |first5=Weimu |last6=Riding |first6=J. |last7=Storm |first7=M. |last8=Minisini |first8=D. |last9=Ullmann |first9=C. |last10=Leng |first10=M. |last11=Leng |first11=M. |title=Astronomical constraints on the duration of the Early Jurassic Pliensbachian Stage and global climatic fluctuations |journal=Earth and Planetary Science Letters |date=2017 |volume=455 |issue=1 |pages=149–165 |doi=10.1016/J.EPSL.2016.08.038 |s2cid=133516849 |url=http://nora.nerc.ac.uk/id/eprint/514816/1/Ruhl_etal_MANUSCRIPT___revised%20Jims%20edit2.pdf }}

The Spinatum regression collides with the worldwide Toarcian Oceanic Anoxic event. The oldest deposits of the sequence (Latest Pliensbachian-Lowermost Toarcian), partly of an age resting on a regional erosional surface, comprise alluvial and deltaic sediments assigned to a number of lithostratigraphic units of local significance. The sequence recovers significant sea-level falls, that are related with the recurrent Late Pliensbachian glaciation, that would be followed at the start of the Toarcian with Global warming and a large scale transgression, recovered locally on the Ciechocinek Formation.{{cite journal |last1=Korte |first1=C. |last2=Hesselbo |first2=S.P. |title=Shallow marine carbon and oxygen isotope and elemental records indicate icehouse–greenhouse cycles during the Early Jurassic |journal=Paleoceanography |date=2011 |volume=26 |issue=1 |page=4219 |doi=10.1029/2011PA002160 |bibcode=2011PalOc..26.4219K |url=https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2011PA002160 |access-date=8 October 2021}}

Thanks to data from the Kaszewy 1 borehole levels of 1200 pCO₂ were recovered, thanks to Plant stomatal index, being the highest amount recovered on the whole Lower Jurassic interval.{{cite journal |last1=Pieńkowski |first1=G. |last2=Hesselbo |first2=S. P. |last3=Barbacka |first3=M. |last4=Leng |first4=M. J. |title=Non-marine carbon-isotope stratigraphy of the Triassic-Jurassic transition in the Polish Basin and its relationships to organic carbon preservation, pCO₂ and palaeotemperature |journal=Earth-Science Reviews |date=2020 |volume=210 |issue=1 |page=103383 |doi=10.1016/j.earscirev.2020.103383 |bibcode=2020ESRv..21003383P |s2cid=224957029 |doi-access=free }} The studied strata also led to know a great variability in Total Organic Content, interpreted as result of a greater terrestrial biodegradation. This led to knowing that the lower temperatures recovered from the Polish Basin in this interval occurred in the latest Rhaetian/earliest Hettangian, the late Hettangian, early Pliensbachian and especially in the Late Pliensbachian (Stokesi, Gibbosus, Spinatum), being this last the coolest period in the whole Early Jurassic.

The Formation strata starts on the Polish Jurassic Depositional sequence V, that besides Drzewica area and Budki–Szydłowiec–Jagodne area, is also known from the Brody-Lubienia borehole (with a massive exposure of the sequence V in an operating quarry near Bielowice, the major one along with Skrzynno near Przysucha), that is located on the eastern part of the Świętokrzyskie Mountains region, giving insight into development of Pliensbachian deposits in the marginal parts of this basin. The initial part of this sequence is associated with a local fall of the sea level, where the lower IV level transition exposes with erosion, on locations such as the Zychorzyn borehole (at depth of 96.1 m) on Drzewica. The latter sedimentation is marked with thin deposits from delta-distributary depositional subsystem, that become thicker around the Budki, where in the zone of the Brody-Lubienia borehole an alluvial-meandering channel deposition system developed. After this initial regression there was a local transgression that led to abundance of local trace fossils and the formation of barrier-lagoonal deposits on Budki and in Brody-Lubienia, along with the increased presence of marine bivalves.{{cite journal |last1=Kopik |first1=J. |title=Faunistic criteria of stratigraphical subdivision of the Lias in North-Western and Central Poland |journal=Wyd. Geol. Warszawa |date=1962 |pages=271–312}}{{cite journal |last1=Kopik |first1=J. |title=Stratigraphy of the Lower Jurassic based on the fauna of the Mechowo IG 1 borehole |journal=Biul. Inst. Geol. |date=1964 |volume=189 |issue=1 |pages=43–55}} In the Brody-Lubienia borehole were developed in embayment-lagoon facies. After the major marine transgression there was a visible change on Budki–Szydłowiec–Jagodne, shifting to fluvial discharge continuously moving along the Nowe Miasto–Iłża fault to the NE direction during the Pliensbachian times. At this time on the Jagodne 1 borehole it was deposited the development of a barrier-lagoon linked with a delta.{{cite journal |last1=Pieńkowski |first1=G. |title=The Lower Jurassic: Sequence stratigraphy and sedimentology |journal=Prace Państwowego Instytutu Geologicznego |date=1997 |volume=153 |issue=1 |pages=217–235}}

The Depositional sequence VI starts on the Jagodne 1 borehole with very large Mud clasts, pointing to intensive erosion of the underlying lagoonal sediments, while on the basin center, on the Zychorzyn borehole the erosion on lower sediments was lesser aggressive. The sediments that were deposited at the start of this sequence are uniformly represented by coarse alluvial deposits, interpreted as meandering river with possible conspicuous share of bed load transport. On the Budki 1 borehole series of coarse-grained alluvial package (especially large scale tabular cross-bedding sets dominate and quartz pebbles association), can represent low-sinuosity braided channels. Another transgressive phase on this sequence led to the formation of foreshore/shoreface/barrier deposits, and a local event on the Polish Basin, where

there was a rapid drowning of the palEvelina Bertoli (born 8 July 1986 in Rome, Italy) is an Olympic Italian eventing rider.{{Cite web|url=https://www.fei.org/athlete/10004113/BERTOLI-Evelina|title = Evelina Bertoli|website=FEI.org}} She competed at the 2021 and 2023 European Championships, and at the 2022 World Championships in Pratoni del Vivaro.{{Cite web|url=https://www.cavallomagazine.it/sport-equestri/completo/ranieri-ed-evelina-la-storia-che-non-si-ferma|title =Ranieri ed Evelina: la storia che non si ferma|website=Cavallo Magazine|date=20 September 2022|language=Italian}} Her sister Sara Bertoli took part in the 2008 Olympic Games in Modern Pentathlon.{{citation needed|date= July 2024}}

In 2024 she competed at the 2024 Summer Olympics in Paris.{{Cite web|url=https://parigi2024.coni.it/en/italia-team/athletes/scheda_atleta/2337:EVELINA_BERTOLI.html|title =Evelina Bertoli|website=Parigi2024.coni.it|accessdate=27 July 2024}} paleorelief with alluvial valleys and coastal plains, resulting in embayed coastline with detached beach andor barrier ridges. There was equilibrium with the sea level, with periodical little regressions and transgressions. The maximum flooding range of this phase is represented by the Szydłowiec sandstones, developed on a regressive period where on Śmiłów was developed an eolian dune depositional subsystem linked with a barrier-lagoon, know due to the presence of barrier crest eolian deposits with plants buried. In this environment, the major Tracksites of the formation were developed. Linked with the Śmiłów Quarry sandstone appear deltaic deposits on the Brody-Lubienia borehole and on Zychorzyn.

The Depositional sequence VII is the last Pliensbachian major sequence, know especially from the Brody-Lubienia borehole and the continuation of an alluvial portion exposed also at Śmiłów, where an exposure exhibits sequence VI/VII characters, showing that the sea level fall was not so significant, as it was in the base of the previous sequence. This sequence starts with a rise of sea level and quick drowning of the whole area, destroying the previous delta system/marsh subsystem development measured at the Brody-Lubienia borehole, that shows that the amplitude of this transgression was quite high, as is represented by a thickness of 16 m.

There are several Types off Seashore Stratification seen on the Drzewica Formation. Starting with the post-Spinatum regression derived shore prograding cycle, where the nearshore deposits show detailed Hummocky cross-stratification, at the time are covered by thin beach-welded facies showing irregular “massive” bedding and numerous Plant roots penetrating down from the undulated bounding surface. Superimposed are fine grained, very well sorted sandstones with giant tabular Cross-bedding set interpreted as beach (Backshore depositional subsystem) Eolian Dune with complete Plant remains buried in the wind-transported Sand (Mostly, Herbaceous-Built Plants). The Direction of the Wind sedimentation is clearly visible on these deposits, where the stratification of the sand is well oriented. Those deposits are abundant on the Antecki quarry. The most related to the shores, probably barrier-Lagoon and Delta depositional systems are clearly visible on the Smilów Quarry, where the exposure shows different lithofacies and strata, including fine-grained, white and light-grey sandstones with Hummocky cross-stratification, with a series of tabular and trough Cross-bedding sets, probably related to near marine depositional subsystem. A more fine-medium-grained, grey to brownish sandstones also with flat-tabular-horizontal bedding with abundant drifted Plant Fossils and plant remains in situ is considered to be part of a clear foreshore barrier–Eolian depositional subsystem, probably related to a series of Dune fields, related to the Sea Barriers. Kaolinized grey Mudstones with abundant Dispersed plant roots are related to more lagoonal depositional subsystems. The slightly smaller and fine built, brownish and yellow sandstones that show details Cross-bedding are related to a more alluvial deposition, probably from the influence of a local Channel. On the Main Smilów Quarry the dominant shore face depositional subsystem show detailed marks of clear Palaeocurrent directions, dispersed trough Cross-bedding inclinations that point to the West. There have been measurements of the Wave-formed ripple that approximately reflects a shoreline orientation. Thanks to the wave ripple crests orientation and the orientation of fossil tree logs it was indicated an inclination of the inclined tabular Foreset bed continuing across the whole outcrop. These Foreset bed show a more pronounced inclination thanks to seaward-dipping Clinoforms, what reflects the original inclination of a barrier slope, with the sum of palaeocurrent pointing to south-west.

Zaosie Anticline-Jeżów Anticline are two of the three structures selected as having the best conditions for geological {{CO2}} storage in the Bełchatów region, with several wells drilled.{{cite journal |last1=Feldman-Olszewska |first1=A. |last2=Adamczak |first2=T. |last3=Szewczyk |first3=J. |title=Charakterystyka poziomów zbiornikowych i uszczelniających w obrębie struktur Zaosia i Jeżowa pod kątem geologicznego składowania {{CO2}} na podstawie danych z głębokich otworów wiertniczych |journal=Biuletyn Państwowego Instytutu Geologicznego |date=2010 |volume=439 |issue=1 |pages=17–28 |url=http://yadda.icm.edu.pl/baztech/element/bwmeta1.element.baztech-a06a3bf4-1705-4329-9a8d-917eceeb9dde |access-date=8 October 2021}} Both the structures are characterized by similar geological feature and petrophysical parameters of rocks, being potential reservoirs. Significant thickness, good reservoir properties and proper depth give sufficient grounds to select the Lower Jurassic sandstone levels of the Drzewica Formation.

Budziszewice-Zaosie structure is one of the potential {{CO2}} storage sites for the biggest emitter of that gas in Europe, the Bełchatów Power Plant, with the major and most perspective reservoir located on the Drzewica Formation Strata locally.{{cite journal |last1=Machowski |first1=W. |last2=Papiernik |first2=B. |title=Model dynamiczny zatłaczania {{CO2}} do dolnojurajskich formacji solankowych struktury Budziszewice-Zaosie |journal=Geopetrol |date=2010 |volume=12 |issue=1 |pages=367–371 |url=http://yadda.icm.edu.pl/yadda/element/bwmeta1.element.baztech-c0639d4f-9776-4b28-93d2-93627d7740c1 |access-date=8 October 2021}} Archival seismic sections subject to secondary interpretation made it possible for a more accurate mapping of the deep structure of the anticline and its definition as present state of recognition as tectonically continuous. The Major drilling hole was stablished on the top of the upper Pliensbachian, JPl3 (the top of the Drzewica formation of the first potential reservoir), with the top of the Ostrowiec formation ({{Langx|pl|seria ostrowiecka}}) as the second potential reservoir. Parametric models of variability were made for the resulting geometrical matrix lithology, contamination, effective porosity and total permeability of the complexes. Several works based on static 3D model recovered effective storage capacity c.a. 10 Mt (during 6 or 30 years of injection depending on hydrodynamic conditions). Other major {{CO2}} storage is found on Sierpc anticline ("Upper Sławęcin Beds"), specially on the Sierpc 2 borehole, with measured capacity of 260 tonnes of dihydrogen.{{cite journal |last1=Luboń |first1=K. |last2=Tarkowski |first2=R. |title=Influence of capillary threshold pressure and injection well location on the dynamic {{CO2}} and {{chem|H|2}} storage capacity for the deep geological structure |journal=International Journal of Hydrogen Energy |date=2021 |volume=46 |issue=58 |pages=30048–30060 |doi=10.1016/j.ijhydene.2021.06.119 |s2cid=237800917 |doi-access=free }}

File:Pinkiert-Katz.jpg

The sandstones of the Drzewica Formation have been object of mining since the Middle Ages, used as key material for the local construction.{{cite journal |last1=Złonkiewicz |first1=Z. |last2=Fijałkowska-Mader |first2=A. |title=Kamień w architekturze zespołu kościelno-klasztornego na Karczówce w Kielcach (Góry Świętokrzyskie) |journal=Przegląd Geologiczny |date=2018 |volume=66 |issue=7 |pages=421–435 |url=https://geojournals.pgi.gov.pl/pg/article/view/26962 |access-date=8 October 2021}} Two kinds are distinctive, the main Szydłowiec sandstones and the Kunów sandstones, mined on Śmiłów (13th century–recent), Kunów (17th–20th century). It

was used by members of the Polish renaissance such as Jan Michałowicz, for some of their most well known pieces, such as the Tomb of Wolski Brothers. Kunów sandstones have also been studied as potential geotourism attractions.

{{Paleobiota-key-compact}}

Along the Early Jurassic, there was a mostly marginal-marine (mainly Mesohaline), deltaic and continental sedimentation that prevailed in the area of Poland. A marine basin of Polyhaline character conditions occurred mainly in the Pliensbachian, due to a flooding of the Polish Basin.{{cite journal |last1=Pieńkowski |first1=G. |last2=Waksmundzka |first2=M. |title=Palynofacies in Lower Jurassic epicontinental deposits of Poland: tool to interpret sedimentary environments |journal=Episodes |date=2009 |volume=32 |issue=1 |pages=21–32 |doi=10.18814/epiiugs/2009/v32i1/004 |s2cid=131735991 |url=https://www.researchgate.net/publication/335747676 |access-date=12 October 2021|doi-access=free }} Due to that, Pliensbachian sedimentation in Pomerania developed in a shelf basin that attained depths of about 100 m, below the storm wave base. As the latest Pliensbachian began, the climate changes to a more cold environment, as prove the presence of ice sheets on northern latitude facies of the same age. That led to changes in salinity. The Drzewica Formation was influenced by an ancient swampy-lagoonal sub-system, with Deltaic currents depositing fluvial sediments. The Main Boreholes show eustatic changes on the marine conditions, with a retreat of the sea level, leading to the appearance of vegetation and abundant pollen on the uppermost parts of the formation. The regressive phase of sea level is represented by the Komorowo Beds and Upper Sławęcin Beds along with the own Drzewica Formation. As the level of the sea recovered on the Toarcian, most of the setting turn out to be a bathyal marine bottom.{{cite journal |last1=Feldman-Olszewska |first1=A. |title=Depositional systems and cyclicity in the intracratonic Early Jurassic basin in Poland |journal=Geological Quarterly |date=1997 |volume=41 |issue=4 |pages=475–490 |url=https://gq.pgi.gov.pl/article/view/8223/pdf_315 |access-date=12 October 2021}} The major outcrop of the formation, found on the Śmiłów Quarry represents a nearshore, deltaic, barrier-lagoonal ecosystem, where the biota left a high report of footprints (+200), with different sizes, that range from small to large animals of various groups. The Smilow Quarry Tracksite is the main outcrop and setting for the Footprints. Along with the coeval (also belonging to the formation) Wólka Karwicka tracksite represent the only ones recovered from the Late Liassic of Europe. The footprints are related to mostly lagoon-derived facies, unlike the vegetation, that appears on Deltaic facies. Brackish deposits are relates to Brachiopodans and other molluscs and Limuloid animals. The presence of Late Pliensbachian common ammonoids and several vertebrate clades connects the marine fauna with similar environments of the same age across Europe. The Drzewica Fauna is also, one of the few from the Pliensbachian-Toarcian Anoxic event recorded worldwide, specially referred to the vertebrate fauna reported.{{cite journal |last1=Branski |first1=P. |title=The mineralogical record of the Early Toarcian stepwise climate changes and other environmental variations (Ciechocinek Formation, Polish Basin) |journal=Volumina Jurassica |date=2012 |volume=10 |issue=10 |pages=1–24 |url=https://yadda.icm.edu.pl/baztech/element/bwmeta1.element.baztech-d4edfc60-55a1-41f6-a7d2-7459ad0d6bdb |access-date=12 October 2021}}

Unidentified blackish bivalves were reported from the formation on the first report of the Tracksites. Are related with shallow lagoonal facies.

Unidentified fin spines are known from this formation.

There are traces of root plants with numerous plant remains, some of them vertically preserved, and on this basis he derived a possible dune-related origin of these sediments.{{cite journal |last1=Karaszewski |first1=W. |last2=Kopik |first2=J. |title=The Stratigraphy of the Mesozoic in the margin of the Góry Świętokrzyskie. Lower Jurassic |journal=Prace Instytutu Geologicznego |date=1970 |volume=56 |issue=1 |pages=65–98}} The plants in the growth position were present at the bases of aeolian sandstone bodies, up to 2 m thick, which wedge out laterally and are covered by argillaceous strata of coastal lagoon origin with drifted plant remains. Mostly of the plant remains are composed by rhizoids and undeterminable fragments, recovered at the Szydłowiec sandstones, Śmiłów and Mirzec, near Starachowice. More recent studies suggest an environment of shallow seafront and beach, which of course does not exclude the presence of Aeolian zones there. Lithofacies on the Smilów Quarry shows slightly inclined beach forests and abundant plant roots in a series of barrier foreshore, backshore and/or aeolian dune facies, that include even plants buried in whole dunes, while drifted plant fossils and tree logs occur on the main depositional surface. This inclined surface exposes most likely a long period of non deposition and washed plants, recovering at the same time the original tilt of the local beach.

File:Drzewica Formation Flora.jpg Flora, probably revorked from the first]]

This flora comes from layers of the also Pliensbachian Gielniów Formation ({{Langx|pl|seria gielniowska}}) (Marginal Brackish), yet is very likely derived from the coeval Drzewica Formation deposits (Coeval coastline) of the Subsequence V. This flora includes at least 30 species: Neocalamites hoerensis (Calamitaceae Equisetales, also found on the Podkowiński Quarry); Laccopteris angustiloba & Phlebopteris muensteri (Matoniaceae ferns); Dictyophyllum acutilobum, Hausmannia crenata, Clathropteris meniscoides & Thaumatopteris schenkii (Dipteridaceae Ferns); Todites williamsonii & Cladophlebis denticulata (Osmundaceae ferns); Pterophyllum subaequale & Nilssonia orientalis/acuminata/simplex (Bennettitales, with Nilssonia being dominant like in the Lublin Floras); Ctenis nilssoni (Cycads); Sagenopteris nilssoniana (Caytoniaceae Seed Ferns); Ginkgoites marginatus (Ginkgos); Ixostrobus siemiradzkii & Czekanowskia nathorstii/setacea (Czekanowskiales Ginkgoopsids); Hirmeriella muensteri (Cheirolepidiaceae conifers); Schizolepis follini/moelleri/braunii & Palissya sp. (Palissyaceae conifers); Podozamites angustifolius/gramineus/stobieckii/distans (Krassiloviaceae conifers).

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The Kaszewy Coals found mostly on the Kaszewy-1 borehole and Niekłan PIG-1 borehole are the major coals of the Drzewica Formation and Ciechocinek Formation, representing the Pliensbachian-Toarcian boundary.{{cite journal |last1=Pointer |first1=R. |title=Fire & Global Change During Key Intervals of the Late Triassic & Early Jurassic with a Focus on the Central Polish Basin |journal=University of Exeter |date=2019 |url=https://ore.exeter.ac.uk/repository/bitstream/handle/10871/36963/PointerR.pdf?sequence=1&isAllowed=y |access-date=12 October 2021}} The Pliensbachian section of the Kaszewy-1 borehole comprises ~220 m of terrestrial and shallow marine siliciclastic sediments.

This Section was located on a nearshore-deltaic influenced setting, with an increased amount of both terrestrial and marine organic matter, reflecting increased weathering and increased transport of terrestrial organic matter, with ups and downs of the amount of both marine and terrestrial matter. Here were collected fossil Charcoal in abundance and polycyclic aromatic hydrocarbon. Total fossil charcoal abundance is generally low in the Pliensbachian part of the study section, before peaking immediately above the Pl-To Boundary. The abundance of coarse fossil charcoal particles (>125 μm) in the Pliensbachian-Toarcian sections of the Kaszewy-1 core is very low (0-15 particles/10 g sediment), while fine fossil charcoal abundance is generally low in the Pliensbachian level. There is also a greater abundance of non-charcoal particles. At the start of the Toarcian locally, there is a measured increase on the amount of fine charcoal particles reflecting changes on the environment. Inside the Polycyclic Aromatic Hydrocarbons, the Pyrolytics (Benz-Anthracene, Benzo(k)Fluoranthene, Fluoranthene, Indeno[1,2,3-cd]Pyrene, Phenanthrene and Pyrene) were detected on a high variety of samples, with the Phenanthrene as the most abundant component, while Coronene is the lowest, suggesting an origin for this last one on the pyrolysis of organic matter. Petrogenics are more abundant on the local coal samples than the Pyrolytic, what can suggest that these last ones may not reflect particularly local high levels of wildfire activity. Apparently, the Kaszewy-1 borehole did not experience increased wildfire activity, but instead that the fine fossil charcoal abundance and Pyrolytics concentration records have shown a more clear regional wildfire signal. The fossil charcoal abundance and geochemical data from Pliensbachian and Toarcian samples show evidence of at least four, and possible another two, levels of increased wildfire activity, and that these can be grouped into two larger periods of increased wildfire activity.

The Drzewica Formation belongs to the Horstisporites planatus (Pl) Zone (Upper Sinemurian – Pliensbachian). This level starts on the older upper part of the Ostrowiec Formation, the Łobez Formation and Komorowo Formation of Pomerania and in other equivalent units from all Poland.{{cite journal |last1=Marcinkiewicz |first1=T. |last2=Fijałkowska-Mader |first2=A. |last3=Pieńkowski |first3=G. |title=Megaspore zones of the epicontinental Triassic and Jurassic deposits in Poland–overview. Biuletyn Państwowego |journal=Instytutu Geologicznego |date=2014 |volume=457 |issue=7 |pages=15–42 |url=https://geojournals.pgi.gov.pl/bp/article/view/29268}} This Megaspore section of relatively poor compared with the lower and upper sections, with the lower boundary of the level is determined by the appearance of the indicator species Horisporites planatus (Selaginellaceae) and The upper limit of the level is marked by the appearance of continuous occurrences of Paxillitriletes phyllicus (Isöetaceae), indicating more humid conditions, and Erlansonisporites sparassis (Selaginellaceae). This level has a series of characteristic megaspores, such as Minerisporites institus (Isöetaceae) and Hughesisporites pustulatus (Lycophyta) and on a minor ratio, rare occurrences of Hughesisporites planatus recorded even above the level range. Is important to recover that the limit of the Pliensbachian-Toarcian in Poland was the first precisely defined on the basis of a detailed stratigraphic-sequential correlation, fully later confirmed by a high-resolution chemostratigraphic correlation, based on isotope analysis, with the ranges of individual megaspores fitting well into this limit. This level can be correlated with the non-megasporous level of Kuqaia quadrata, found in the sediments of the Sinemurian- Lower Pliensbachian Yangxia Formation in the Xinjiang Province, China.

In the Polish profiles, the Pl level correlates with the upper part of Rogalska's 1st phase as well as the 2nd and 3rd microflora phase, where the following indicator miospores appear: Lycopodiumsporites gristhorpensis (Lycopodiaceae), Undulatisporites undulapolus (Filicopsida) and Applanopsipollenites segmentatus (Gymnospermopsida), and in central Poland represents the works of the Upper Sinemurian and the whole Pliensbachian, being probably correlated with the middle part of the miospore level Cerebropollenites macroverrucosus (Coniferophyta), distinguished in the Pliensbachian and Toarcian deposits in northern Europe.

The Drzewica Formation palynoflora is recovered mostly on the Gutwin and Brody-Lubienia boreholes, and includes the next plant groups: Bryophyta, Lycopodiaceae, Equisetaceae, Selaginellaceae, Cyatheaceae, Dipteridaceae, Dicksoniaceae, Gleicheniaceae, Matoniaceae, Osmundaceae, Schizeaceae, Peltaspermaceae, Taxodiaceae, Cheirolepidiaceae, Araucariaceae, Podocarpaceae, Pinaceae, Gnetales, Cycadidae, Bennettitales and Ginkgoales.{{cite journal |last1=Rogalska |first1=M. |title=Stratigraphy of the Lower and Middle Jurassic in the Polish Lowlands on the basis of spore and pollen analysis. [Stratygrafia Jury Dolnej i Srodkowej na Obszarze Nizu Polskiego na Podstawie badan sporowo-pylkowych] |journal=Prace Instytut Geologiczny |date=1976 |volume=78 |issue=1 |pages=5–61}} In between all the taxa, Pollen from Seed Ferns and Conifers dominate over miospores, indicating a relatively dry ecosystem. Freshwater algae miospores are known (Botryococcus sp., Cymatiosphaera sp.), as well Paleozoic palynoremains washed from uplands (Walchia sp., Pseudowalchia biangulina, Ullmannia frumentaria, Florinites antiquus, etc.), what indicate a clear active river influx, yet has also evidence of marine ingressions due to the presence of saltwater acritarchs (Psophosphaera coniferoides, Leiosphaeridia sp.).

Beyond proper palynogy, biomass associated has been recovered, specially on the Brody-Lubenia borehole, with abundance of C29 diasterenes (>70%), that proves a great contribution of land plants and thus terrestrial deposits nearby. There is also in some levels abundance of algae-derived C27 and C28 diasterenes, coeval with acritarchs, prasinophytes and dinoflagellates, being this last ones important primary producers in the Polish Basin. The presence of C27 sterols points to the importance of the dinoflagellates, but also other groups, such as Bangiophyceae and Eustigmatophyceae algae or marine protists like the Thraustochytriaceae. At least in some facies there is evidence of proliferation of freshwater-tolerant algae in the brackish environments of the Polish Basin.

The Lublin Upland fluvial sandstones contain diverse types of fossil flora, associated genera and species only with Lower Jurassic sediments. Originally, while studying the Carboniferous flora from the boreholes in the area of the planned Bogdanka Coal Mine, appeared typical flora in similar to Jurassic formations.{{cite journal |last1=Migier |first1=T. |title=Nowe stanowiska flory jurajskiej w Lubelskim Zagłębiu Węglowym |journal=Materiały III Naukowej Konferencji Paleontologów poświęconej badaniom regionu górnośląskiego oraz karbonu LZW i GZW. Streszczenia komunikatówUniwersytet Śląski, Katowice |date=1978 |volume=78 |pages=33–34}} The age of the plant material was not determined concretely until 2020, where was recovered as being Pliensbachian-Toarcian in age, with the flora representing an arid environment, more probably Pliensbachian, that is covered locally by the Drzewica Formation.{{cite journal |last1=Ruebsam |first1=W. |last2=Pieńkowski |first2=G. |last3=Schwark |first3=L. |title=Toarcian climate and carbon cycle perturbations–its impact on sea-level changes, enhanced mobilization and oxidation of fossil organic matter |journal=Earth and Planetary Science Letters |date=2020 |volume=546 |issue=1 |page=546 |doi=10.1016/j.epsl.2020.116417 |bibcode=2020E&PSL.54616417R |s2cid=224911816 |url=https://www.sciencedirect.com/science/article/pii/S0012821X20303617 |access-date=13 October 2021}} The Brody-Lubienia borehole is abundant on terrestrial Palynomorphs (know due to the presence of C29 Diasterenes, >70%), but also has high abundances of aquatic derived biomass. Even with that, there is a clear consensus with the more terrestrial character of the sediments from Brody-Lubienia, expressed by the frequent occurrence of plant roots and paleosol horizons. This also is recovered on the rate of MTTCs (mono-, di- and tri-methyl-trimethyltridecyl-chromanes) where higher indices at Brody-Lubienia indicate lower salinities and a stronger influx of riverine freshwater. The environment was probably Dry, developing flora on the near Freshwater influx settings. The Lublin Flora is linked with the flowing waters from the East.

Lublin lias is dominated by cycads and Bennetites Ginkgoales and seed ferns occur sporadically, all on a conglomerate with numerous species occurs in the bottom, where the deposits are filled with of coal, mudstone, sandstone and clay siderite (reworked from the Carboniferous), as well as pebbles from Devonian limestones. Vegetation mostly grew outside the sedimentation area, as well as on shores and shallows.{{cite journal |last1=Szydeł |first1=Z. |last2=Szydeł |first2=R. |title=Profil utworów liasu na obszarze Lubelskiego Zagłębia Węglowego |journal=Przegląd Geologiczny |date=1981 |volume=29 |issue=11 |pages=568–571 |url=https://geojournals.pgi.gov.pl/pg/article/view/18493/14643 |access-date=13 October 2021}}

At the Śmiłów Quarry, plant remains are known, and are interpreted as derived from an aeolian rework, with the plants buried in growth position by barrier crest aeolian dunes.{{cite journal |last1=Pacyna |first1=G. |title=Matoniaceous ferns preserved in growth position in Lower Jurassic dune sandstones of the Holy Cross Mountains (Poland) |journal=Annales Societatis Geologorum Poloniae |date=2020 |volume=91 |issue=2 |page=241 |url=https://geojournals.pgi.gov.pl/asgp/article/view/32974/24155 |access-date=13 October 2021}} Szydłówek quarry host also a nearshore-foreshore-backshore/eolian setting, where the flora is dominated by woody trunks, plant root moulds and impressions of drifted woody trunks, that suggest the presence of large coniferous forests around the Szydłówek tracksite. Plants here thrive on the foredune are exposed to salt spray, strong wind, and burial by blowing and accumulating sand. Ferns like Matonia braunii maybe worked as dune stabilisers, like the extant plant Leymus arenarius.

• List of fossiliferous stratigraphic units in Poland
• List of dinosaur-bearing rock formations

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• Blue Lias, England
• Charmouth Mudstone Formation, England
• Sorthat Formation, Denmark
• Hasle Formation, Denmark
• Zagaje Formation, Poland
• Ciechocinek Formation, Poland
• Borucice Formation, Poland
• Rotzo Formation, Italy
• Saltrio Formation, Italy
• Moltrasio Formation, Italy
• Marne di Monte Serrone, Italy
• Calcare di Sogno, Italy
• Podpeč Limestone, Slovenia
• Coimbra Formation, Portugal
• El Pedregal Formation, Spain
• Fernie Formation, Canada
• Whiteaves Formation, British Columbia
• Navajo Sandstone, Utah
• Aganane Formation, Morocco
• Tafraout Group, Morocco
• Azilal Formation, Morocco
• Budoš Limestone, Montenegro
• Kota Formation, India
• Cañadón Asfalto Formation, Argentina
• Los Molles Formation, Argentina
• Kandreho Formation, Madagascar
• Elliot Formation, South Africa
• Clarens Formation, South Africa
• Evergreen Formation, Australia
• Cattamarra Coal Measures, Australia
• Hanson Formation, Antarctica
• Mawson Formation, Antarctica

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{{reflist|colwidth=30em}}

Category:Jurassic Poland

Category:Jurassic System of Europe

Category:Pliensbachian Stage

Category:Sandstone formations

Category:Mudstone formations

Category:Alluvial deposits

Category:Deltaic deposits

Category:Shallow marine deposits

Category:Ichnofossiliferous formations

Category:Fossiliferous stratigraphic units of Europe

Category:Paleontology in Poland