Meinhold, Guido

[["dc.bibliographiccitation.firstpage","1367"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","Geological Magazine"],["dc.bibliographiccitation.lastpage","1372"],["dc.bibliographiccitation.volume","157"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Roberts, Nick M. W."],["dc.contributor.author","Arslan, Arzu"],["dc.contributor.author","Jensen, Sören"],["dc.contributor.author","Ebbestad, Jan Ove R."],["dc.contributor.author","Högström, Anette E. S."],["dc.contributor.author","Høyberget, Magne"],["dc.contributor.author","Agić, Heda"],["dc.contributor.author","Palacios, Teodoro"],["dc.contributor.author","Taylor, Wendy L."],["dc.date.accessioned","2021-04-14T08:24:32Z"],["dc.date.available","2021-04-14T08:24:32Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.1017/S0016756820000564"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/81321"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.eissn","1469-5081"],["dc.relation.issn","0016-7568"],["dc.title","U–Pb dating of calcite in ancient carbonates for age estimates of syn- to post-depositional processes: a case study from the upper Ediacaran strata of Finnmark, Arctic Norway"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2051"],["dc.bibliographiccitation.issue","12"],["dc.bibliographiccitation.journal","Geological Magazine"],["dc.bibliographiccitation.lastpage","2066"],["dc.bibliographiccitation.volume","157"],["dc.contributor.author","Palacios, Teodoro"],["dc.contributor.author","Högström, Anette E. S."],["dc.contributor.author","Ebbestad, Jan Ove R."],["dc.contributor.author","Agić, Heda"],["dc.contributor.author","Høyberget, Magne"],["dc.contributor.author","Jensen, Sören"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Taylor, Wendy L."],["dc.date.accessioned","2021-04-14T08:27:52Z"],["dc.date.available","2021-04-14T08:27:52Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.1017/S001675682000031X"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/82432"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.eissn","1469-5081"],["dc.relation.issn","0016-7568"],["dc.title","Acritarchs from the Duolbagáisá Formation (Cambrian Series 2, Miaolingian) on the Digermulen Peninsula, Finnmark, Arctic Norway: towards a high-resolution Cambrian chronostratigraphy"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","289"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","GFF"],["dc.bibliographiccitation.lastpage","294"],["dc.bibliographiccitation.volume","141"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Högström, Anette E. S."],["dc.contributor.author","Ebbestad, Jan Ove R."],["dc.contributor.author","Jensen, Sören"],["dc.contributor.author","Palacios, Teodoro"],["dc.contributor.author","Høyberget, Magne"],["dc.contributor.author","Agić, Heda"],["dc.contributor.author","Taylor, Wendy L."],["dc.date.accessioned","2020-04-03T12:56:23Z"],["dc.date.available","2020-04-03T12:56:23Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1080/11035897.2019.1583685"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/63606"],["dc.relation.issn","1103-5897"],["dc.relation.issn","2000-0863"],["dc.title","A late Caledonian tectono-thermal event in the Gaissa Nappe Complex, Arctic Norway: evidence from fine-fraction K‒Ar dating and illite crystallinity from the Digermulen Peninsula"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.journal","Geological Magazine"],["dc.bibliographiccitation.lastpage","22"],["dc.contributor.author","Agić, Heda"],["dc.contributor.author","Högström, Anette E.S."],["dc.contributor.author","Jensen, Sören"],["dc.contributor.author","Ebbestad, Jan Ove R."],["dc.contributor.author","Vickers-Rich, Patricia"],["dc.contributor.author","Hall, Michael"],["dc.contributor.author","Matthews, Jack J."],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Høyberget, Magne"],["dc.contributor.author","Taylor, Wendy L."],["dc.date.accessioned","2022-04-01T10:00:52Z"],["dc.date.available","2022-04-01T10:00:52Z"],["dc.date.issued","2021"],["dc.description.abstract","Abstract New occurrences of flask-shaped and envelope-bearing microfossils, including the predominantly Cambrian taxon Granomarginata , are reported from new localities, as well as from earlier in time (Ediacaran) than previously known. The stratigraphic range of Granomarginata extends into the Cambrian System, where it had a cosmopolitan distribution. This newly reported Ediacaran record includes areas from Norway (Baltica), Newfoundland (Avalonia) and Namibia (adjacent to the Kalahari Craton), and puts the oldest global occurrence of Granomarginata in the Indreelva Member (< 563 Ma) of the Stáhpogieddi Formation on the Digermulen Peninsula, Arctic Norway. Although Granomarginata is rare within the assemblage, these new occurrences together with previously reported occurrences from India and Poland, suggest a potentially widespread palaeogeographic distribution of Granomarginata through the middle–late Ediacaran interval. A new flask-shaped microfossil Lagoenaforma collaris gen. et sp. nov. is also reported in horizons containing Granomarginata from the Stáhpogieddi Formation in Norway and the Dabis Formation in Namibia, and flask-shaped fossils are also found in the Gibbett Hill Formation in Newfoundland. The Granomarginata – Lagoenaforma association, in addition to a low-diversity organic-walled microfossil assemblage, occurs in the strata postdating the Shuram carbon isotope excursion, and may eventually be of use in terminal Ediacaran biostratigraphy. These older occurrences of Granomarginata add to a growing record of body fossil taxa spanning the Ediacaran–Cambrian boundary."],["dc.identifier.doi","10.1017/S0016756821001096"],["dc.identifier.pii","S0016756821001096"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/105535"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-530"],["dc.relation.eissn","1469-5081"],["dc.relation.issn","0016-7568"],["dc.title","Late Ediacaran occurrences of the organic-walled microfossils Granomarginata and flask-shaped Lagoenaforma collaris gen. et sp. nov."],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","204"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","GFF"],["dc.bibliographiccitation.lastpage","212"],["dc.bibliographiccitation.volume","135"],["dc.contributor.author","Lehnert, Oliver"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Arslan, Arzu"],["dc.contributor.author","Ebbestad, Jan Ove R."],["dc.contributor.author","Calner, Mikael"],["dc.date.accessioned","2018-11-07T09:23:47Z"],["dc.date.available","2018-11-07T09:23:47Z"],["dc.date.issued","2013"],["dc.description.abstract","The Stumsnas 1 core, drilled in 2011 in the southern part of the Siljan Ring, provides new insights into the stratigraphy of the Ordovician succession in central Sweden. The core section shows evidence of the structural complications caused by the late Devonian meteorite impact in the area. In the core, about 90m of Tremadocian to Darriwilian strata are sandwiched between Proterozoic igneous basement rocks. At the lower contact, the sedimentary succession starts with glauconitic, fine-grained siliciclastics and carbonates directly resting on the weathered basement. The basal siliciclastic unit is overlain by a ca. 19-m-thick limestone succession, well-known from this part of the Baltoscandian Basin, includes strata corresponding to the Latorp Limestone through the upper Holen Formation. This succession is covered by a limestone-marl alternating sequence, representing some yet unknown deeper water facies, presumably coeval to the topmost Holen Formation through upper Dalby Limestone. The upper third of the sedimentary succession in the core includes numerous slices of partly overturned strata, including relatively thick successions of the Slandrom Formation, Fjacka Shale and Jonstorp Formation, as well as carbonate and siliciclastic units of yet unknown stratigraphic origin."],["dc.identifier.doi","10.1080/11035897.2013.813582"],["dc.identifier.isi","000323317400007"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/29666"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Taylor & Francis Ltd"],["dc.relation.issn","2000-0863"],["dc.relation.issn","1103-5897"],["dc.title","Ordovician stratigraphy of the Stumsnas 1 drill core from the southern part of the Siljan Ring, central Sweden"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1253"],["dc.bibliographiccitation.issue","11"],["dc.bibliographiccitation.journal","Canadian journal of earth sciences"],["dc.bibliographiccitation.lastpage","1261"],["dc.bibliographiccitation.volume","55"],["dc.contributor.author","Jensen, Sören"],["dc.contributor.author","Högström, Anette E.S."],["dc.contributor.author","Høyberget, Magne"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","McIlroy, Duncan"],["dc.contributor.author","Ebbestad, Jan Ove R."],["dc.contributor.author","Taylor, Wendy L."],["dc.contributor.author","Agić, Heda"],["dc.contributor.author","Palacios, Teodoro"],["dc.date.accessioned","2020-12-10T18:37:21Z"],["dc.date.available","2020-12-10T18:37:21Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1139/cjes-2018-0035"],["dc.identifier.eissn","1480-3313"],["dc.identifier.issn","0008-4077"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76925"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","99"],["dc.bibliographiccitation.journal","Precambrian Research"],["dc.bibliographiccitation.lastpage","110"],["dc.bibliographiccitation.volume","328"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Jensen, Sören"],["dc.contributor.author","Høyberget, Magne"],["dc.contributor.author","Arslan, Arzu"],["dc.contributor.author","Ebbestad, Jan Ove R."],["dc.contributor.author","Högström, Anette E.S."],["dc.contributor.author","Palacios, Teodoro"],["dc.contributor.author","Agić, Heda"],["dc.contributor.author","Taylor, Wendy L."],["dc.date.accessioned","2020-12-10T15:20:54Z"],["dc.date.available","2020-12-10T15:20:54Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1016/j.precamres.2019.04.014"],["dc.identifier.issn","0301-9268"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72851"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","First record of carbonates with spherulites and cone-in-cone structures from the Precambrian of Arctic Norway, and their palaeoenvironmental significance"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","87"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","GFF"],["dc.bibliographiccitation.lastpage","98"],["dc.bibliographiccitation.volume","134"],["dc.contributor.author","Lehnert, Oliver"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Bergstroem, Stig M."],["dc.contributor.author","Calner, Mikael"],["dc.contributor.author","Ebbestad, Jan Ove R."],["dc.contributor.author","Egenhoff, Sven"],["dc.contributor.author","Frisk, Asa M."],["dc.contributor.author","Hannah, Judith L."],["dc.contributor.author","Hogstrom, Anette E. S."],["dc.contributor.author","Huff, Warren D."],["dc.contributor.author","Juhlin, Christopher"],["dc.contributor.author","Maletz, Joerg"],["dc.contributor.author","Stein, Holly J."],["dc.contributor.author","Sturkell, Erik"],["dc.contributor.author","Vandenbroucke, Thijs R. A."],["dc.date.accessioned","2018-11-07T09:15:09Z"],["dc.date.available","2018-11-07T09:15:09Z"],["dc.date.issued","2012"],["dc.description.abstract","New drill cores from the largest known impact structure in Europe, the relict of the Siljan meteorite crater, provide new possibilities to reconstruct Early Palaeozoic marine environments and ecosystems, and to document changes in sedimentary facies, sea level and palaeoclimate in Baltoscandia. The impact crater is an important target of the project \"Concentric Impact Structures in the Palaeozoic\" within the framework of the \"Swedish Deep Drilling Program\". Two core sections, Mora 001 and Solberga 1, have been analysed. The sedimentary successions of these core sections include strata of late Tremadocian through late Wenlock ages. Our preliminary studies show not only that several of the classical Palaeozoic units of Sweden are represented in the area, but also that other significantly different facies are preserved in the Siljan district. An erosional unconformity representing a substantial hiatus occurs between Middle Ordovician limestone and a Llandovery-Wenlock (Silurian) shale succession in the western part of the Siljan structure and suggests an extended period of uplift and erosion. This may be related to forebulge migration due to flexural loading by the Caledonian thrust sheet to the west. Thus, this part of Sweden, previously regarded as a stable cratonic area, presumably was affected by the Caledonian collision between Baltica and Laurentia."],["dc.identifier.doi","10.1080/11035897.2012.692707"],["dc.identifier.isi","000306600000002"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/27607"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Taylor & Francis Ltd"],["dc.relation.issn","1103-5897"],["dc.title","New Ordovician-Silurian drill cores from the Siljan impact structure in central Sweden: an integral part of the Swedish Deep Drilling Program"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.journal","Geological Magazine"],["dc.bibliographiccitation.lastpage","22"],["dc.contributor.author","Ebbestad, Jan Ove R."],["dc.contributor.author","Hybertsen, Frida"],["dc.contributor.author","Högström, Anette E. S."],["dc.contributor.author","Jensen, Sören"],["dc.contributor.author","Palacios, Teodoro"],["dc.contributor.author","Taylor, Wendy L."],["dc.contributor.author","Agić, Heda"],["dc.contributor.author","Høyberget, Magne"],["dc.contributor.author","Meinhold, Guido"],["dc.date.accessioned","2022-01-11T14:05:38Z"],["dc.date.available","2022-01-11T14:05:38Z"],["dc.date.issued","2021"],["dc.description.abstract","Abstract Sabellidites cambriensis is a tubular non-mineralized metazoan that appears as compressed ribbon-shaped imprints with transverse wrinkling, thick walls and an even tube diameter of up to 3 mm. The distribution of Sabellidites is investigated in three Ediacaran–Cambrian sections on the Digermulen Peninsula in Arctic Norway, spanning the Manndrapselva Member of the Stáhpogieddi Formation and the lower member of the Breidvika Formation. Here, the Ediacaran–Cambrian boundary is located in the lower part of the upper parasequence (third cycle) of the Manndrapselva Member. Specimens of Sabellidites are rare but consistently present close to the lowest level of Treptichnus pedum and upsection, whereas the taxon is common and abundant in the lower part of the lower member of the Breidvika Formation, with an upper record at c. 55 m above the base. The range is comparable with that of the GSSP section in Newfoundland, Canada, establishing Sabellidites as an index fossil for the lowermost Cambrian. In the Manndrapselva Member, Sabellidites co-occurs with the acritarch Granomarginata , indicative of the lowermost Cambrian Granomarginata Zone, whereas in the Breidvika Formation it co-occurs with Asteridium . Sabellidites is widely distributed in Baltica, through the Rovnian and Lontovan regional stages but confined to the Fortunian global stage. In its lower range, Sabellidites is associated with a Treptichnus pedum trace fossil association and a depauperate leiosphaerid acritarch assemblage, followed by a Granomarginata assemblage. In its upper range, Sabellidites co-occurs with acritarchs of the Asteridium–Comasphaeridium Zone and the tubular foraminiferan Platysolenites . In Baltica, Sabellidites is a useful index fossil."],["dc.description.abstract","Abstract Sabellidites cambriensis is a tubular non-mineralized metazoan that appears as compressed ribbon-shaped imprints with transverse wrinkling, thick walls and an even tube diameter of up to 3 mm. The distribution of Sabellidites is investigated in three Ediacaran–Cambrian sections on the Digermulen Peninsula in Arctic Norway, spanning the Manndrapselva Member of the Stáhpogieddi Formation and the lower member of the Breidvika Formation. Here, the Ediacaran–Cambrian boundary is located in the lower part of the upper parasequence (third cycle) of the Manndrapselva Member. Specimens of Sabellidites are rare but consistently present close to the lowest level of Treptichnus pedum and upsection, whereas the taxon is common and abundant in the lower part of the lower member of the Breidvika Formation, with an upper record at c. 55 m above the base. The range is comparable with that of the GSSP section in Newfoundland, Canada, establishing Sabellidites as an index fossil for the lowermost Cambrian. In the Manndrapselva Member, Sabellidites co-occurs with the acritarch Granomarginata , indicative of the lowermost Cambrian Granomarginata Zone, whereas in the Breidvika Formation it co-occurs with Asteridium . Sabellidites is widely distributed in Baltica, through the Rovnian and Lontovan regional stages but confined to the Fortunian global stage. In its lower range, Sabellidites is associated with a Treptichnus pedum trace fossil association and a depauperate leiosphaerid acritarch assemblage, followed by a Granomarginata assemblage. In its upper range, Sabellidites co-occurs with acritarchs of the Asteridium–Comasphaeridium Zone and the tubular foraminiferan Platysolenites . In Baltica, Sabellidites is a useful index fossil."],["dc.identifier.doi","10.1017/S0016756821001187"],["dc.identifier.pii","S0016756821001187"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/97710"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-507"],["dc.relation.eissn","1469-5081"],["dc.relation.issn","0016-7568"],["dc.rights.uri","http://creativecommons.org/licenses/by/4.0"],["dc.title","Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]