Höganäs Formation
{{Short description|Late Triassic to Early Jurassic geologic formation in Sweden}}
{{Infobox rockunit
| name = Höganäs Formation
| image =Sgff a 1907442 f0011 c.jpg
| caption =Paleoenvironment Reconstruction
| type = Geological formation
| age = Rhaetian-Hettangian
~{{fossilrange|202|199}}
| period = Hettangian
| prilithology = Sandstone
| otherlithology = Shale, coal
| namedfor =
| region = Skåne
| country = {{SWE}}
| coordinates = {{coord|56.1|N|12.7|E|display=inline,title}}
| paleocoordinates = {{coord|44.6|N|8.5|E|display=inline}}
| unitof = Ängelholm Trought
| subunits = Bjuv, Helsingborg & Vallåkra members
| underlies = Rya Formation
| overlies = Kågeröd Formation
| thickness = 200 m
| extent =
| area =
| map = {{Location map+ | Sweden
| relief = 1
| width = 250
| float = center
| places =
{{Location map~ | Sweden
| lat_deg = 56.1
| lon_deg = 12.7
| mark = Blue pog.svg
| marksize = 12
}}
}}
| map_caption =
}}
The Höganäs Formation is a Late Triassic to Early Jurassic geologic formation in Skåne, Sweden. The formation is mostly known for its incredible flora collection from the Bjuv member, composed of over 110 species, and also includes several vertebrate remains, such as fishes, amphibians and dinosaur tracks & remains, although none have yet been referred to a specific genus.Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. It´s regional equivalent is the Zagaje Formation in Poland.{{Cite journal |last1=Gierliński |first1=Gerard |last2=Pieńkowski |first2=Grzegorz |last3=Niedźwiedzki |first3=Grzegorz |date=2004 |title=Tetrapod Track Assemblage in the Hettangian of Sołtyków, Poland, and its Paleoenvironmental Background |url=http://dx.doi.org/10.1080/10420940490444861 |journal=Ichnos |volume=11 |issue=3–4 |pages=195–213 |bibcode=2004Ichno..11..195G |doi=10.1080/10420940490444861 |issn=1042-0940}}
Description
The Höganas Formation was deposited in what is now the southern part of Sweden Skåne. The formation straddles the Triassic-Jurassic boundary and has provided evidence of widespread mire-forest deterioration that began in the latest Rhaetian.Petersen & Lindström, 2012, p.8 The upper part of the Höganas Formation is correlated with the Rønne Formation of Bornholm, which is administered by Denmark. The Hóganas Formation is rich in coal and has provided many fossil flora.Petersen & Lindström, 2012, p.9
=Vallåkra Member=
This member represent the basal part of the Formation, that represents a transition between the terrestrial Kågeröd Formation and the delta dominated coal layers of the Bjuv Member, being made by poorly stratified clay & claystone, mostly green in coloration.{{cite journal |last1=Sivhed |first1=Ulf |title=Litho-and biostratigraphy of the Upper Triassic-Middle Jurassic in Scania, southern Sweden|journal=Sveriges geologiska undersökning |date=1984 |volume=31 |issue=12 |pages=31–50 |url=http://resource.sgu.se/produkter/c/c806-rapport.pdf |access-date=11 February 2021}} The sediments of this member are exposed mostly in the quarry of the town of the same name, where is subdivided on the next levels: 6 m of mixed layers, whose composition includes material seen both on the Kågeröd Formation and this member (red clay and 5 m light clay, 3 m argillaceous sandstone and l m dark clay and several layers composed by Spherosiderite). The uppermost levels are covered by the coal seams of the Bjuv Member. This member has been considered as of Middle and Upper Rhaetian in age.{{cite book |last1=Troedsson |first1=G.T. |title=On rhythmic sedimentation in the Rhaetic-Liassic beds of Sweden |date=1950 |publisher=lnt. Geol. Congr. Rep. XVIII S ession |location=London |pages=64–72 |edition=1 |url=https://paleoarchive.com/literature/Troedsson1950-RhythmicSedimentationRhaeticLiassicSweden.pdf |access-date=12 December 2021}}
=Bjuv Member=
The second member is the Bjuv Member, known as the most fossiliferous one, that was known originally as the Gruv Member (gruva= mine).{{cite journal |last1=Bölau |first1=E. |title=Der Sudwest- und Slidostrand des Ballisehen Schildes (Schonen und Ostbaltikum) |journal=Geologiska Föreningen i Stockholm Förhandlingar |date=1959 |volume=7 |issue=1–2 |pages=167–230|doi=10.1080/11035895909449146 }} Coal and clay have been mined in this area since the fifteenth century, being this intensive mining one of the main reasons the fossiliferous layers have provided such a diverse flora. The Bjuv member is divided on two different seams, the B seam, that overlies the older member and the A seam, that marks the limit with the Helsingborg Member. This layer has a thickness of around 37.22 and 45.72 m in bore No. 256 (stored at the Höganäs Company in Bjuv) from the Bjuv area. The layer is dominated by coarse arenaceous sediments, specially between Billesholm and Höganäs, parallel to the Söderåsen and Kullaberg horsts. Towards the southern part of this area the deposition changes, with an increased abundance of argillaceous contents, specially at places like Skromberga. The age of this member is considered to be Late Rhaetian-Lower Hettangian. The Plant fossils found at this layer are one of the main fossil material of the whole Mesozoic in Sweden, composed by more than 110 species, one of the most complete floras of the same age from any location.{{cite journal |last1=Lundblad |first1=Britta |title=Rhaeto-Liassic floras and their bearing on the stratigraphy of Triassic-Jurassic rocks |journal=STHLM. Contrib. Geol. |date=1959 |volume=16 |issue=1 |pages=83–102}} The main reason for this datation where suggested due to the presence of the plants Lepidopteris ottonis and Thaumatopteris shenki, as well palynological samples that suggested a Middle Rhaetian age (the Rhaetipollis-Limbosporites Miospore Zone).{{cite journal |last1=Nathorst |first1=A.G. |title=Om floran i Skånes kolförande bildningar. l. Floran vid Bjuf |journal=Sver. Geol. Unders. |date=1878–1886 |volume=27 |issue=33 |pages=0–131 |url=https://resource.sgu.se/dokument/publikation/c/c29rapport/c29-rapport.pdf |access-date=12 December 2021}} Latter works have fount that the Dinosaur Footprint layers spam between the Rhaetian-Hettangian boundary. Beyond the exceptional flora, the member is also known for fossils of Molluscs, arthropods and fish remains.
=Helsingborg Member=
The Uppermost member of the formation is entirely of Hettangian age, and is the last layer before the start of the deposition of the younger dominant marine Rya Formation. This member is dominated by Deltaic sediments, along several marine interealatians are frequent, with deposition of coarse, in some cases arkosic sandstones in between
more fine-grained deposits may indicate Early Kimmerian tectonic movements.{{cite journal |last1=Norling |title=Post-Palaeozoic Tectonics of Scania. In Bergström el al.: Guide to excursions in Scania |journal=Sver. Geol. Unders. Ca |date=1982 |volume=54 |issue=1 |pages=28–48}} The member has a maximunn thickness of 215 m and is divided in 2 parts: Höllviken No. 2 indicated that the lower part starts with up to 12 m of kaolinitic clay succeeded by a 15–20 m thick sequence of cross-bedded arkoses and light-coloured clays, being called Boserup beds or Thaumatopteris schenki zone (Pinuspollenites-Trachysporites Miospore Zone).{{cite journal |last1=Hermelin |first1=S.G. |title=Anmärkningar om Boserups Stenkols-Grufva, och de öfvriga Stenkolsförsök uti Skåne |journal=Kungl. V et. Akad. Hand! |date=1773 |volume=1 |issue=1 |pages=236–254}}{{cite journal |last1=Lund |first1=J. |title=Rhaetic to Lower Liassic palynology of the onshore south-eastern North Sea Basin |journal=Danm. G Eol. U Nders., II Raekke |date=1977 |volume=109 |issue=1 |page=128 |url=https://geusjournals.org/index.php/raekke2/article/view/6900 |access-date=12 December 2021}} by Lund ( 1977) This beds are known from Boserup, but also from the central part of Helsingborg, the Köpinge No. 3 bore and even extent to the Höganäs region (northwest to Eslöv in the south). This beds are overlain by some metres of arenaceous clays, iron claystone and calcareous sandstone with few intercalation of a coal seam (known as Tågaborg coal seam), where floral remains are also recovered such as Dictyophyllum nilssoni and Equisetites spp.. Then the layers turn into 5 m of argillaceous sandstone and 5 m slightly arenaceous clays, with a last 1 m of calcareous sandstone, on a sequence known from cliff series at Laröd-Sofiero at the north of Helsingborg, with plant remains such as Nilssonia polymorpha and Dictyophyllum nilssoni, referred to the Pinuspallenites-Trachysporites zone. It also appears on Rosendal, Fleninge, Farhult and Klappe. Helsingborg (Vossbäumer I 969). There is a coal seam, Tinkarpsflötsen, in the
middle part of the sequence. The upper part of the Helsingborg Member starts with a 28 m thick sandstone, with a section known as Fleninge beds, that represent layers where marine ingressions were more common, with the last layers of the formation made up of sandstone, claystone and several minor coal seams.
Fossil content
= Ichnofossils =
{{Paleobiota-key-compact}}
{{div col|colwidth=25em}}
- Lockeia siliquaria (Bivalves){{cite journal |last1=Pieńkowski |first1=G. |title=Eustatically-controlled sedimentation in the Hettangian-Sinemurian (Early Jurassic) of Poland and Sweden |journal=Sedimentology |date=1991 |volume=38 |issue=3 |pages=503–518 |doi=10.1111/j.1365-3091.1991.tb00364.x |bibcode=1991Sedim..38..503P |url=https://www.researchgate.net/publication/229858779 |access-date=12 December 2021}}
- Planolites annularis (Polychaetes)
- Planolites montanus (Polychaetes)
- Diplichnites isp. (Xiphosurans, Insects, Arachnids)
- Teichichnus isp. (Polychaetes, Echiurans, Holothurians.)
- Skolithos isp. (Polychaetes, Phoronidans)
- Monocraterion tentaculatum (Polychaeta, Sipuncula, Enteropneustans & Echiurans)
- Rhizocorallium isp. (Polychaeta, Sipuncula, Enteropneustans & Echiurans)
- Aulichnites isp. (Gastropods)
- Diplocraterion parallelum (Polychaeta, Sipuncula, Enteropneustans & Echiurans)
{{div col end}}
=Annelida=
| class ="wikitable" align="center" width="100%" |
| Genus
! Species ! Stratigraphic position ! Member ! Material ! Notes ! Images |
|---|
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" | Cocoons | style="background:#D1FFCF;" | Freshwater Clitellata Cocoons (Oligochaeta and Hirudinea), identified with palynological residues, and through to be tridimensional nets of probable algal origin. Fragmentary mesh-like networks of happiness threads composed of homogenous translucent material. They show the outer wall (hapsine) construction specific to clitellate annelids and lack an alytine (inner) layer. A disorderly meshwork of the hapsine layer and hapsine fibers of unequal thickness, are diagnostic of the type species Dictyothylakos pesslerae. The cocoons Dictyothylakos pesslerae resemble specially those of modern Leechs, and are common on flooded basin sediments, which implies not only the presence of parasitic leeches, but also the presence of large hosts nearby, as has been confirmed by Dinosaur Footprints | |
| style="background:#D1FFCF;" |
"Cycadeospermum"{{cite journal |last1=Svein |first1=B. |last2=Mahendra |first2=N. Bose |last3=Roy |first3=T. Sawyer |title=Clitellate cocoons in freshwater deposits since the Triassic |journal=Zoologica Scripta |date=1991 |volume=20 |issue=4 |pages=347–366 |doi=10.1111/j.1463-6409.1991.tb00300.x |s2cid=83998036 |url=https://d1wqtxts1xzle7.cloudfront.net/38117856/Manum__Bose_and_Sawyer_1991_Clitellate_Cocoons_in_freshwater_deposits_since_Triassic._Zool_Scripta_20__437-366-with-cover-page-v2.pdf?Expires=1641738942&Signature=W6CMu72jwgqXUcUGZPtOWzhwrtk3~SIr4Y9y84iTZvvacl2bLhgz934WDXem9rQdMbAzs0rrOggz9fqK8JCPFu-6MJhNBnSPkW0zXGxlhbAoT38RZHRWe4tGY8lQSLWhZ3LsNsnzhAX5P9Y0RYqyDxWfAoDZ~rtqiyBsHMBaO1uruA-hQPlCW1hRlPULQ6pq7EOagT2w5B6cPSOik9vrYBn1o2Xo55Vnykb1yftW99SDBXp11sEsGgSm4V6CE-Lmu9xwCyj6At46CklfAxTySG~sqWoNIgUmZpyeINB8rdon-sHzYb6nmmSW5vyVYWW9gRfK9XP3n3xCGuAFySa5Xg__&Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA |access-date=8 September 2021 |archive-date=9 January 2022 |archive-url=https://web.archive.org/web/20220109135133/https://d1wqtxts1xzle7.cloudfront.net/38117856/Manum__Bose_and_Sawyer_1991_Clitellate_Cocoons_in_freshwater_deposits_since_Triassic._Zool_Scripta_20__437-366-with-cover-page-v2.pdf?Expires=1641738942&Signature=W6CMu72jwgqXUcUGZPtOWzhwrtk3~SIr4Y9y84iTZvvacl2bLhgz934WDXem9rQdMbAzs0rrOggz9fqK8JCPFu-6MJhNBnSPkW0zXGxlhbAoT38RZHRWe4tGY8lQSLWhZ3LsNsnzhAX5P9Y0RYqyDxWfAoDZ~rtqiyBsHMBaO1uruA-hQPlCW1hRlPULQ6pq7EOagT2w5B6cPSOik9vrYBn1o2Xo55Vnykb1yftW99SDBXp11sEsGgSm4V6CE-Lmu9xwCyj6At46CklfAxTySG~sqWoNIgUmZpyeINB8rdon-sHzYb6nmmSW5vyVYWW9gRfK9XP3n3xCGuAFySa5Xg__&Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA |url-status=dead }} | style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" |
| style="background:#D1FFCF;" | Cocoons | style="background:#D1FFCF;" | Freshwater Clitellata Cocoons (Oligochaeta and Hirudinea), identified with palynological residues. Also called "red eggs" and present on the estuarine series of Yorkshire | rowspan="2" | File:Cocoon of Hirudo verbana.jpg File:Placobdella papillifera (YPM IZ 059049).jpeg, example of leech]] |
| style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" |
|style="background:#D1FFCF;" | Cocoons |style="background:#D1FFCF;" | Freshwater Clitellata Cocoons (Oligochaeta and Hirudinea), identified with palynological residues, and through to be tridimensional nets of probable algal origin. Fragmentary mesh-like networks of happiness threads composed of homogenous translucent material. |
=Bivalves=
| class = "wikitable" |
| Genus
! Species ! Location ! Stratigraphic position ! Material ! Notes ! Images |
|---|
| Cardinia
| C. ingelensis |
|
| Isolated Shells | A Clam, member of Cardiniidae inside Carditida. | |
| Eutrapetzium
| E. pullastra |
|
| Isolated Shells | An Oyster, member of Ostreidae inside Ostreida. The local material assigned to this genus is now lost | |
| Liostrea
| L. hisingeri |
|
| Isolated Shells | An Oyster, member of Ostreidae inside Ostreida. The most common Bivalve found locally, indicator of increased salinity levels on the Hettangian layers. | File:Liostrea socialis 783.jpg specimens]] |
| Modiolus
| M. hoffinanni |
|
| Isolated Shells | A Mussel, member of Mytilidae inside Mytilida. | |
=Insecta=
=Sharks=
| class = "wikitable" |
| Genus
! Species ! Location ! Stratigraphic position ! Material ! Notes ! Images |
|---|
| Hybodus
|H. sp. |
|
|
|A freshwater/marine shark, member of Hybodontidae inside Hybodontiformes |File:Hybodus model.jpg reconstruction]] |
| Lissodus{{cite journal |last1=Fischer |first1=J. |title=Brief synopsis of the hybodont form taxon Lissodus Brough, 1935, with remarks on the environment and associated fauna |journal=Freiberger Forschungshefte |date=2008 |volume=528 |issue=1 |pages=1–23 |url=https://lup.lub.lu.se/luur/download?func=downloadFile&recordOId=2365890&fileOId=3131925 |access-date=22 January 2022}}
| Lissodus sp. |
|
|
| A freshwater/marine shark, member of Lonchidiidae inside Hybodontiformes. | |
| style="background:#E3F5FF;" |
Palaeoxyris{{Cite journal |last1=Krüger |first1=Ashley |last2=Slater |first2=Sam |last3=Vajda |first3=Vivi |date=2021-07-03 |title=3D imaging of shark egg cases (Palaeoxyris) from Sweden with new insights into Early Jurassic shark ecology |journal=GFF |volume=143 |issue=2–3 |pages=229–247 |doi=10.1080/11035897.2021.1907442 |s2cid=237716825 |issn=1103-5897|doi-access=free }} | style="background:#E3F5FF;" | P. muensteri | style="background:#E3F5FF;" |
| style="background:#E3F5FF;" |
| style="background:#E3F5FF;" |
| style="background:#E3F5FF;" | A freshwater shark, likely produced by members of Hybodontidae. Originally identified as Spirangium, considered gigantic Chara, fresh-water green algae (stone-worths). The palynological and palynofacies data points to a predominantly freshwater depositional environment, with the eggs are found in close association with Neocalamites hoerensis stems (An ideal substrate for hybodont sharks to attach their eggs to). | style="background:#E3F5FF;" | |
| Parvodus
|P. sp. |
|
|
|A freshwater/marine shark, member of Lonchidiidae inside Hybodontiformes | |
=Bony Fish=
=Amphibia=
| class="wikitable" align="center" |
| Genus
!Species !Location !Stratigraphic position !Material !Notes !Images |
|---|
| Gerrothorax{{cite journal |last1=Nilsson |first1=T. |title=A new find of Gerrothorax rhaeticus Nillson, a plagiosaurid from the Rhaetic of Scania |journal=Lunds Universitates Arsskrift |date=1946 |volume=42 |issue=10 |pages=1–49 |url=https://paleoarchive.com/literature/Nilsson1946-NewGerrothoraxRhaeticusScania.pdf |access-date=12 December 2021}}
| G. pulcherrimus |
| Bjuv member (Rhaetian) |
| An amphibian, member of the family Plagiosauridae. Represents the only major tetrapod macrofossil from this layers. | File:Gerrothorax BW.jpg reconstruction]] |
=Dinosauria=
Tracks discovered in the Höganäs Formation have been assigned to the ichnogenus Grallator (Eubrontes) cf. giganteus, which were discovered in Rhaetian strata, and Grallator (Eubrontes) soltykovensis, which were discovered in Hettangian strata.{{citation |last1=Gierliński |first1=G. |last2=Ahlberg |first2=A. |year=1994 |title=Late Triassic and Early Jurassic dinosaur footprints in the Höganäs Formation of southern Sweden |journal=Ichnos |volume =3 |issue=2 |pages=1–99 |doi=10.1080/10420949409386377}} A few of the tracks were taken to museums, but most of them disappeared in natural floodings.
After the end of a seven-year excavation project at Billesholm, researchers announced on 13 October 2022 the identification of seven dinosaur species based on fossil remains, out of which three species were new to science.{{Cite news |last=Melin |first=Simon |date=2022-10-13 |title=Unika fyndet: Tre nya dinosaurier upptäckta i Billesholm |language=sv |work=SVT Nyheter |url=https://www.svt.se/nyheter/lokalt/helsingborg/tre-nya-dinosaurier-upptackta-i-billesholm |access-date=2022-10-13}} The fossils are yet to be analyzed and scientifically published.{{Cite web |title=Dinosauriefynd i Skåne skriver om historien |url=https://www.aftonbladet.se/a/O8rRQE |access-date=2022-10-13 |website=Aftonbladet |date=12 October 2022 |language=sv}}
See also
References
{{Reflist|2}}
= Bibliography =
- {{citation |last1=Petersen |first1=Henrik I. |last2=Lindström |first2=Sofie |year=2012 |title=Synchronous Wildfire Activity Rise and Mire Deforestation at the Triassic–Jurassic Boundary |journal=PLoS ONE |volume=7 |issue=10 |pages=1–15 |doi=10.1371/journal.pone.0047236 |doi-access=free |pmid=23077574 |pmc=3471965 }}
- {{citation |last1=Weishampel |first1=David B. |author2-link=Peter Dodson |last2=Dodson |first2=Peter |author3-link=Halszka Osmólska |last3=Osmólska |first3=Halszka |year=2004 |title=The Dinosauria, 2nd edition |url=https://books.google.com/books?id=vtZFDb_iw40C |publisher=Berkeley: University of California Press |pages=1–880 |access-date=2019-02-21 |isbn=0-520-24209-2 |author1-link=David B. Weishampel }}
{{Mesozoic Sweden|state=expanded}}
{{DEFAULTSORT:Hoganas Formation}}
Category:Geologic formations of Sweden
Category:Jurassic System of Europe
Category:Triassic System of Europe
Category:Ichnofossiliferous formations