GFF

Papers
(The TQCC of GFF is 4. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-06-01 to 2025-06-01.)
ArticleCitations
Sandbian (Late Ordovician) conodonts in Estonia: distribution and biostratigraphy17
The development of dark shales from the middle and late Cambrian to early Ordovician on the East European Platform – with focus on Gotland11
Upper Ordovician carbon isotope chemostratigraphy and a high-resolution assessment of the Hirnantian Stage in the Baltic Sea subsurface8
First discovery of Small Shelly Fossils and new occurrences of brachiopods and trilobites from the early Cambrian (Stage 4) of the Swedish Caledonides, Lapland7
Emendment to the term complex in: “Guide for geological nomenclature in Sweden” (Kumpulainen 2016)7
The youngest known tommotiid: Lapworthella bornholmiensis (Poulsen, 1942) from Cambrian Stage 4 to Guzhangian (Miaolingian) strata of Bornholm and southern Sweden7
Musculature of an Ordovician (Darriwilian) patelliform gastropod from Estonia6
First record of an Early Ordovician brachiopod and conodont fauna from Lapland, Sweden5
Inversion tectonics in the Sorgenfrei–Tornquist Zone: insight from new marine seismic data at the Bornholm Gat, SW Baltic Sea5
Rock fracturing by subglacial hydraulic jacking in basement rocks, eastern Sweden: the role of beam failure5
Introducing palaeolithobiology5
High diversity and early radiation of organic-walled phytoplankton in southern Baltica during the Middle-Late Ordovician – evidence from the Borenshult-1 drillcore of southern Sweden5
Neutron tomography, fluorescence and transmitted light microscopy reveal new insect damage, fungi and plant organ associations in the Late Cretaceous floras of Sweden4
The Middle Ordovician Jinonicella (Mollusca) from Belarus and Ukraine4
U-Pb baddeleyite age for the Ottfjället Dyke Swarm, central Scandinavian Caledonides: new constraints on the timing of the Baltoscandian Dyke Swarm, opening of the Iapetus Ocean and Neoproterozoic gla4
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