-
An, Pengcheng; Krystyn, Leopold; Wang, Yongdong & Kürschner, Wolfram Michael
(2023).
Integrated stratigraphy of Carnian deposits in the
Dinaric Alps, Glamoc (SW Bosnia-Hercegovina).
-
Tekin, Kagan; Krystyn, Leopold; Kürschner, Wolfram Michael; Okuyucu, Cengiz; Sayit, Kan & Forel, Marie-Béatrice
(2023).
Integrated stratigraphy (from radiolarians, conodonts, palynomorphs, ammonoids, ostracods) of the Early Carnian deepening upward sequence (the Huglu Unit) within the tectonic slices/blocks of the Mersin Melange, southern Turkey: biochronologies and paleogeographic implications.
-
Kürschner, Wolfram Michael
(2022).
Discussion of Stomata frequency analysis as a proxy for palaeo-atmospheric CO2 reconstructions.
-
Bang, Emil; Smelror, Morten; Kürschner, Wolfram Michael & Nakrem, Hans Arne
(2021).
Palynology of Early Cretaceous hydrocarbon seep carbonates from Wollaston Forland, Northeast Greenland – preliminary results.
-
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Zaputlyaeva, Alexandra; Mazzini, Adriano; Blumenberg, M; Scheeder, Georg; Kürschner, Wolfram Michael & Kus, J
[Vis alle 8 forfattere av denne artikkelen]
(2020).
Timing – an underestimated key factor for source rock evaluation, case study from NE Java, Indonesia.
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Gravendyck, Julia; Bachelier, Julien B.; Kürschner, Wolfram Michael & Herendeen, Patrick S.
(2020).
(009) A proposal to solve a paradox when neotypifying names of fossil‐taxa.
Taxon.
ISSN 0040-0262.
69(3).
doi:
10.1002/tax.12249.
Fulltekst i vitenarkiv
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Labes, Alienor; Mazzini, Adriano; Akhmanov, Grigorii G. & Kürschner, Wolfram Michael
(2020).
Palynology of Holocene Lake Baikal sediments.
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Kürschner, Wolfram Michael
(2019).
A review of Late Triassic and Early Jurassic palynology.
Vis sammendrag
The Late Triassic is characterized by enhanced rates of biotic turnover in the marine and terrestrial realms
culminating in the End-Triassic extinction. Several negative C-isotope anomalies have been reported that indicate
coeval pertubations in the carbon cycle. An integrated approach using physical, bio - and chemostratigraphic
tools is pivotal to improve correlations between regions across different latitudes and constrain rates of biotic
and environmental changes. In this contribution I review palynological data with emphasis on the Carnian and
Triassic – Jurassic intervals from different sections in Europe and Scandinavia and discuss their stratigraphic
correlation and environmental significance.
-
-
Baranyi, Viktoria & Kürschner, Wolfram Michael
(2018).
A comparision of the North American and European Carnian and Norian palynofloras.
-
Kürschner, Wolfram Michael
(2018).
On the Biological Significance of Pollen and Spore Tetrads.
-
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Kürschner, Wolfram Michael; van Soelen, Elsbeth Ester; Rusinovich, Ales & Suprunenko, Oleg
(2018).
Palynostratigraphy and Carbon Isotope Stratigraphy of the
Permian-Triassic Strata in the Timan-Pechora basin.
Vis sammendrag
The Timan–Pechora Basin is a complex of rift basins and a series of foreland basins along the Uralian orogenic
front on the east margin of the basin. The Permian-Triassic (PT) strata were studied in 4 cores located alongside
an East-West transect from the eastern Barents Sea into the eastern part of the Pechora sea including the Kolguyev
Island. 25 sediment samples were analyzed for palynology, palynofacies and C-isotope composition of the bulk
sedimentary organic matter. The aim of the present study was to establish a constrained stratigraphic correlation of
the Permian/Triassic transition in the Norwegian and Russian Arctic sector as well as the Uralian foreland basin.
The Upper Permian – Lower Triassic sediments comprise shallow marine to continental mixed siliciclastic
sediments (sand-, silt- and mudstones) that are deposited on a shallow shelf with deltaic complexes to coastal plain
environment with fluvial-estuarine sediments. All samples show a C-isotope composition of about -26 to -27 permille.
We did not find a negative C isotope excursion which is normally characteristic for the PT boundary interval.
Some of the mud-siltstone samples yielded well preserved palynomorph assemblages dominated by taeniate and
bisaccate pollen and spores. The maturity of the organic matter is low, TAS 1-2. The palynofacies is dominated by
wood remains, cuticle fragments and some degraded amorphous matter characteristic for fluvio-deltaic sediments.
The presence of acritarchs indicate a marine influence in a neritic depositional environment. Reduviasporonites
and taeniate pollen (Weylandites, Vittatina) are indicative for the PT boundary interval. However, so far spore
dominated assemblages, as reported from Greenland, the Barents Sea or Svalbard are absent. Our preliminary data
may indicate a sedimentary hiatus at the PT boundary in the Timan-Pechora basin or the absence of PT boundary
features are due to a still rather low sampling density in the cores.
-
Kürschner, Wolfram Michael
(2017).
Late Triassic Environmental changes inferred from palynological and Carbon isotope studies.
-
Kürschner, Wolfram Michael
(2017).
Revisiting the stratigraphic correlation of Tr-J boundary interval – new and old concepts.
-
Iqbal, Shahid; Wagreich, Michael; Jan, Irfan; Kürschner, Wolfram Michael & Gier, Susanne
(2017).
Geochemical evidences for palaeoclimatic fluctuations at the Triassic-Jurassic boundary: southwestern margin of the Neotethys in the Salt Range, Pakistan.
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Kürschner, Wolfram Michael; Iqbal, Shahid; Wagreich, Michael; Jan, Irfan & Gier, Susanne
(2017).
Palynology and Carbon isotope stratigraphy of the Triassic – Jurassic transition in the Salt Range (Pakistan).
-
Grundan, Ekaterina; Kürschner, Wolfram Michael & Wout, Krijgsman
(2017).
Climate variations in the late Miocene – early Pliocene in the Black Sea region (Taman peninsula) inferred from palynological analyses.
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van Soelen, Elsbeth Ester; Peterse, Francien & Kürschner, Wolfram Michael
(2017).
A comparison of bulk versus compound specific C-isotope and palynological data from core 7128/12-U-01: implications for the use of C-isotope chemostratigraphic correlation of the Permian-Triassic boundary interval on the Barents shelf.
-
van Soelen, Elsbeth Ester; Hasic, Edi; Planke, Sverre; Svensen, Henrik; Sleveland, Arve Rein Nes & Midtkandal, Ivar
[Vis alle 8 forfattere av denne artikkelen]
(2017).
Permian-Triassic palynofacies and chemostratigraphy in a core recovered from central Spitsbergen.
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van Soelen, Elsbeth Ester; Peterse, Francien & Kürschner, Wolfram Michael
(2017).
A compound specific carbon isotope record for the late Permian to Early Triassic.
Vis sammendrag
The end Permian biotic crisis is one of the most severe extinction events in the history of the earth. A carbon isotope shift near the Permian-Triassic boundary is an important global stratigraphical tool, showing a negative shift of 5-10‰ over the late Permian extinction phase. However, most records displaying this shift are based bulk carbon isotope values. Since the start of the extinction is characterized in many marine settings by the onset of anoxia, it coincides with a sharp increase in marine derived organic matter. Such a change in palynofacies affects also the δ13CTOC record. Compound, specific isotope analysis (CSIA) can help to improve the δ13C curve and help to estimate the size of the atmospheric carbon-isotope shift, which is thought to result from CO2 release by a large ingenous province (LIP) in Siberia. However, the high maturity of many late Permian sections complicates lipid biomarker work, especially if oil has migrated into the study section. We present data from low mature sediments covering the late Permian to Early Triassic. The sediments were deposited in a shallow marine environment in the Barents Sea and were recovered from the Finnmark plateau by drilling. Long chain n-alkanes (C25-C35) show a strong odd-over-even dominance, and the alkanes likley derive from the leave-waxes of higher terrestrial plants (i.e. trees). In a next step, CSIA on the long chain n-alkanes will help to estimate the magnitude of the change in atmospheric carbon isotope values.
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Kürschner, Wolfram Michael & van Soelen, Elsbeth Ester
(2016).
Permian – Triassic palynology and stratigraphy.
-
Planke, Sverre; Zuchuat, Valentin; Svensen, Henrik; Hammer, Øyvind; Braathen, Alvar & Silkoset, Petter
[Vis alle 27 forfattere av denne artikkelen]
(2016).
Coring and High-Resolution Imaging of the Permian-Triassic Boundary in Deltadalen, Svalbard.
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van Soelen, Elsbeth Ester; Twitchett, Richard & Kürschner, Wolfram Michael
(2016).
END PERMIAN SALINITY AND OXYGENATION CHANGES IN A SHALLOW MARINE BASIN IN EAST GREENLAND.
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Olsen, Paul; Parker, William; Kürschner, Wolfram Michael & Huber, Peter E.
(2016).
Implications of the stratigraphic results of the Colorado Plateau Coring Project (CPCP): salt vs. plate tectonics vs. eustasy in the Late Triassic Chinle Formation.
-
van Soelen, Elsbeth Ester; Planke, Sverre; Svensen, Henrik; Twitchett, Richard; Polozov, Alexander G. & Kürschner, Wolfram Michael
(2016).
Chemo- and palyno-stratigraphy of the Permian-Triassic transition in the Boreal region.
Geophysical Research Abstracts.
ISSN 1029-7006.
-
van Soelen, Elsbeth Ester; Planke, Sverre; Svensen, Henrik; Twitchett, Richard; Polozov, Alexander G. & Kürschner, Wolfram Michael
(2016).
Chemo- and palyno-stratigraphy of the Permian-Triassic transition in the Boreal region.
-
Miller, Charlotte Sarah; Kürschner, Wolfram Michael; Peterse, Francien; Baranyi, Viktoria & Reichart, Gert-Jan
(2016).
The Carnian (Late Triassic) carbon isotope excursion: new insights from the terrestrial realm.
Geophysical Research Abstracts.
ISSN 1029-7006.
-
Miller, Charlotte Sarah; Kürschner, Wolfram Michael; Peterse, Francien; Baranyi, Viktoria & Reichart, Gert-Jan
(2016).
The Carnian (Late Triassic) carbon isotope excursion: new insights from the terrestrial realm.
-
Kürschner, Wolfram Michael & Krystyn, Leopold
(2016).
Integrated stratigraphy of the Carnian biotic crises.
Geophysical Research Abstracts.
ISSN 1029-7006.
18.
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Kürschner, Wolfram Michael & Krystyn, Leopold
(2016).
Integrated stratigraphy of the Carnian biotic crises.
-
Mueller, Steven & Kürschner, Wolfram Michael
(2016).
The Carnian Pluvial Phase in the Boreal.
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Font, Eric; Adatte, Thierry; Planke, Sverre; Svensen, Henrik & Kürschner, Wolfram Michael
(2016).
Impact, volcanism, global changes, and mass extinction.
Palaeogeography, Palaeoclimatology, Palaeoecology.
ISSN 0031-0182.
441,
s. 1–3.
doi:
10.1016/j.palaeo.2015.11.001.
-
Kürschner, Wolfram Michael
(2015).
Atmospheric CO2 and climate history in deep time.
-
Font, Eric; Adatte, Thierry; Planke, Sverre; Svensen, Henrik & Kürschner, Wolfram Michael
(2015).
Impact, volcanism, global changes, and mass extinction.
Palaeogeography, Palaeoclimatology, Palaeoecology.
ISSN 0031-0182.
441,
s. 1–3.
doi:
10.1016/j.palaeo.2015.11.001.
-
Krystyn, Leopold; Richoz, Sylvain; Maslo, Martin; Kürschner, Wolfram Michael; Gardin, Silvia & Gallet, Yves
(2015).
Proposal for a candidate GSSP for the base of the Rhaetian stage at Steinbergkogel (Salzkammergut, Austria).
Berichte Institutes für Erdwissenschaften Karl-Franzen-Univ. Graz.
ISSN 1608-8166.
21,
s. 213–213.
Vis sammendrag
The Steinbergkogel section near Hallstatt, Salzkammergut, Austria is proposed as candidate GSSP for the Norian-Rhaetian boundary (NRB) with the boundary defined in bed 111 of section A, 2m20 above section base by the FAD of Misikella posthernsteini. This definition follows the boundary recommendation of the NRB Task Force of the Subcommission on Triassic Stratigraphy. The Steinbergkogel exposes a pelagic basin facies of red and gray Middle Norian to Lower Rhaetian Hallstatt Limestone with a rich ammonoid and conodont fauna. Accompanying biostratigraphic
boundary markers are the FA of Misikella koessensis, the FA of the ammonoids Paracochloceras suessi and of Sagenites s.str. Despite the overall rare occurrence of Misikella posthernsteini in the early Rhaetian, Bed 111 further
shows a distinct conodonts frequency change from Epigondolella to Misikella dominance as a
valuable proxy for the boundary. An identical, time-correlative shift in conodont biofacies is seen in
the Steinbergkogel quarry sections B and C and in various Tethyan sections from Germany (Berchtesgaden), Austria (Hallstatt, Dachstein, Hernstein), Slovakia (S. Brezova), Turkey (Oyuklu; Mersin), Oman (Musandam; Sumeini, Baid and Al Aqil) and Indonesia (Timor). The FAD of M. posthernsteini occurs 40 cm higher up than the FA of Misikella hernsteini. Just below the FO of Misikella hernsteini is the LO of Metasibirites, a widespread late Norian ammonoid genus
and the worldwide disappearance of Monotis (M. salinaria/subcircularis in low palaeolatitudes and M.
ochotica group in the Boreal). Very rare coccolith spp were observed below the Norian-Rhaetian boundary. They increase in abundance just above the FAD of Misikella posthernsteini where the first Crucirhabdus minutus was also recorded. Above the FAD of M. posthernsteini is also the FA of the
dinoflagellate cyst Rhaetogonyaulax rhaetica, which can be here lithologically controlled, followed by the disappearance of the “Norian” palynomorphs.
Between the FA of M. hernsteini and the FAD of M. posthernsteini lies a magnetic polarity reversal,
ending a relatively long normal polarity interval, which can be recognized in other Tethyan magnetostratigraphies whereas, unfortunately, a clear correlation with the lacustrine Newark magnetochronology remains ambiguous. The delta13Ccarb record is well preserved and shows no
significant variations around the boundary.
The Austrian Salzkammergut region fulfills essential requirements for a Rhaetian GSSP: i) A lithologically uniform boundary interval, good exposure conditions in an old abandoned quarry and location on public land in a mountainous forested area in an UNESCO world heritage site assure longtime preservation and accessibility, ii) the area is well known for diverse Norian-Rhaetian low palaeolatitude invertebrate faunas (cephalopods, bivalves, gastropods, brachiopods, reefal organisms) found in different bathymetric and facial environments; iii) knowledge of their temporal and spatial distribution is now well advanced and a high-resolution correlation framework of the relevant pelagic
biomarkers (ammonoids, conodonts) linked to abiotic stratigraphic tools such as stable isotopes and
magnetostratigraphy has been achieved; iv) the multistratigraphical approach allows a correlation with
the geochronologically constrained Pucara Group in northern Peru where the NRB is dated to around 205,5 my, and in the future hopefully with the astrochronologically tuned time scale of the Newark basin.
-
Kürschner, Wolfram Michael; Müller, Steven & Hounslow, Mark
(2015).
Triassic palynostratigraphy and environmental history: how to correlate the Early Carnian in the Arctic with the Tethys realm.
-
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van Soelen, Elsbeth Ester; Twitchett, Richard & Kürschner, Wolfram Michael
(2015).
Palyno- and chemo-stratigraphy of the Permian-Triassic transition in the Boreal region.
-
van Soelen, Elsbeth Ester; Richard, Twitchett & Kürschner, Wolfram Michael
(2015).
Palynology of the Permian-Triassic transition in East Greenland.
-
Krystyn, Leopold; Richoz, Silvain; Maslo, Martin; Kürschner, Wolfram Michael; Gallet, Yves & Gardin, Stephan
(2015).
Proposal for a candidate GSSP for the base of the Rhaetian stage at Steinbergkogel (Salzkammergut, Austria).
-
Miller, Charlotte Sarah; Fraser, Wesley; Jardine, Phil & Kürschner, Wolfram Michael
(2015).
Quantifying UV-B flux over the Late Triassic Carnian Pluvial Extinction Event (c. 233–229 Ma).
Geophysical Research Abstracts.
ISSN 1029-7006.
17.
-
Miller, Charlotte Sarah; Fraser, Wesley; Jardine, Phil & Kürschner, Wolfram Michael
(2015).
Quantifying UV-B flux over the Late Triassic Carnian Pluvial Extinction Event (c. 233–229 Ma).
-
Mueller, Steven & Kürschner, Wolfram Michael
(2015).
Depositional Environments and Integrated Stratigraphy of the Upper Triassic Kapp Toscana Group on Svalbard and the Barents Sea Shelf.
-
Mueller, Steven; Hounslow, Mark W. & Kürschner, Wolfram Michael
(2015).
Integrated stratigraphy of the Kapp Toscana Group from central Spitsbergen: identification of the Boreal equivalent of the Carnian Pluvial Phase.
-
Kürschner, Wolfram Michael; Mueller, Steven & Hounslow, Mark W.
(2015).
Towards a refined Late Triassic palynostratigraphy in the Boreal region: an example from Carnian Kapp Toscana group on Spitsbergen.
-
Geissler, Wolfram; Knies, Jochen; Nielsen, Tove; Gaina, Carmen; Matthiessen, Jens & Damm, Volkmar
[Vis alle 24 forfattere av denne artikkelen]
(2014).
The Opening of the Arctic-Atlantic Gateway: Tectonic, Oceanographic and Climatic Dynamics - an IODP Initiative.
-
Olsen, Paul; Geissman, John; Kent, Dennis; George, Gerehls; Irmis, Randall & Mundil, Roland
[Vis alle 13 forfattere av denne artikkelen]
(2014).
The Colorado Plateau Coring Project (CPCP): A Continuous Cored Record of Triassic Continental Environmental Change in Western North America.
Vis sammendrag
The Triassic Period (251.9-201.3 Ma) is bound by two of the Earth’s largest mass extinctions, suffered several giant bolide impacts and eruption of 3 large igneous provinces, and witnessed evolution of the main components of modern tetrapod communities, and yet has sparse geochronological calibration. To bridge this gap, NSF- and ICDP-funded coring of Phase 1 of the CPCP finished in 12/2013 with the recovery of two major cores (1A, 518m and 2B, 253m; 31km apart) from opposites sides of Petrified Forest National Park spanning nearly the entire Triassic sequence (Chinle & Moenkopi fms) with many U-Pb datable levels (1,2,3) and a recoverable paleomagnetic polarity record (4). The cores will provide a U-Pb and paleomagnetic exportable time scale and sedimentary and geochemical proxies with undoubted superposition testing the motivating hypotheses of: 1) the accuracy of orbitally-paced cyclicity of the Newark APTS (5); 2) apparent climate trends as a function of drift through climate belts (6) and atmospheric CO2 (7); 3) the temporal link between the mid-Late Triassic biotic turnover and the ~100 km Manicouagan impact (1); and 4) the delayed ecological dominance of dinosaurs coupled to climate-driven provinciality (1,8). For orientation, the cores were drilled using a azimuth-tracking device, deviated 30° and 15° from vertical to the SE and S, and CT-scanned. The unprecedented sedimentological and stratigraphic detail visible in the CT-scans, and geophysical logs, plus the ~100% recovery promises successful tests of the motivating hypotheses and provide a superbly detailed reference section for this key episode in Earth system history.
1, Irmis+,2011, EPSL 309:258; 2, Ramazani+, 2011, GSA Bull. 123:2142; 3, Ramazani+, 2014, AJS 314:981; 4, Steiner & Lucas, 2000, JGR B 105:25791; 5, Kent & Olsen, 1999, JGR 104(B6):12831-12841; 6, Kent and Tauxe, 2005, Science 307:240–244; 7, Schaller+, 2012, EPSL 323-324:27–39; 8, Kent +, 2014, PNAS 111:7958–7963.
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Kürschner, Wolfram Michael
(2014).
Classopollis variability in tetrads and pollen size – implications for palaeopolyploidy among early Jurassic Cheirolepidiaceae
.
-
Kürschner, Wolfram Michael
(2014).
Vegetation and climate change during the Triassic - Jurassic mass extinction - did good genes help plants to survive one of the biggest earth crises?
-
Mueller, Steven & Kürschner, Wolfram Michael
(2014).
Depositional Environments and (Bio-)stratigraphy of the Upper Triassic Kapp Toscana Group on Svalbard and the Barents Sea Shelf.
-
Kürschner, Wolfram Michael & Mueller, Steven
(2014).
Integrated Magneto-, Carbon isotope and quantitative palynostratigraphy of the Upper Triassic Kapp Toscana Group on Spitsbergen, Norway.
-
Mueller, Steven & Kürschner, Wolfram Michael
(2014).
Depositional Environments and (Bio-)stratigraphy of the Upper Triassic Kapp Toscana Group on Svalbard and the Barents Sea Shelf.
-
Kürschner, Wolfram Michael & Mueller, Steven
(2014).
Late Triassic (Carnian) Boreal vegetation and climate history and its relationship with the Wrangellia large igneous province.
Geophysical Research Abstracts.
ISSN 1029-7006.
16.
-
Kürschner, Wolfram Michael & Mueller, Steven
(2014).
Late Triassic (Carnian) Boreal vegetation and climate history and its relationship with the Wrangellia large igneous province.
-
Mueller, Steven & Kürschner, Wolfram Michael
(2013).
Palynostratigraphy of Upper Triassic sections of the Kapp Toscana Group on Central Svalbard.
-
Kürschner, Wolfram Michael; Batenburg, Sietske & Mander, Luke
(2013).
Abberant Classopollis pollen reveal evidence for environmental mutagenesis in conifers during the End-Triassic mass extinction.
-
Mueller, Steven & Kürschner, Wolfram Michael
(2013).
Palynofacies and palynology of the Upper Triassic deposits at the Judvalskampen section (central Spitsbergen).
-
Kürschner, Wolfram Michael
(2013).
Vegetation history through periods of extreme environmental changes.
-
Kürschner, Wolfram Michael; Mander, Luke; Mueller, Steven & Ruhl, Micha
(2013).
Late Triassic palynology in the Alpine and Arctic realm: a review of palynofloral trends and their stratigraphic correlations.
Vis sammendrag
The end – Triassic period is characterized by major faunal turnover that culminated in the extinction of about 25%
of marine and terrestrial families. Palynological records show a more variable decline in floral diversity but overall
pronounced quantitative changes in vegetation composition. Several lines of evidence suggest that the effects of
a major flood basalt volcanism in the Central Magmatic Province and associated environmental changes, such as
rising CO2 and warming, methane release and ocean acidification, were the causes for this biotic crisis. However,
the different scenarios are still controversially discussed. In this contribution we review palynological data from
different sections from the Alpine to the Arctic realm and discuss their stratigraphic correlation and environmental
significance.
-
Michael, Szurlies; Geluk, Mark C.; Wout, Krijgsman; Kürschner, Wolfram Michael & Zeug, Matthias
(2012).
High-resolution base-level cycles and sand dispersal directions around the Permian-Triassic boundary in Western and Central Europe.
-
Hincke, Alexandra J.C.; Hunt, John; Kürschner, Wolfram Michael; Lotter, André F. & Wagner-Cremer, Friederike
(2012).
Stomatal response of Nothofagus fusca (New Zealand red beech) to CO2 availability and nutrient status.
-
Kürschner, Wolfram Michael
(2012).
Variation in pollen size and tetrad configuration in Late Triassic Classopollis as a measure of polyploidy in Cheirolepidaceae.
-
Kürschner, Wolfram Michael
(2011).
Plants in a low CO2 world – an integrated study of plant growth in low CO2 experiments and late glacial fossil remains.
-
Schneebeli-Hermann, Elke; Hochuli, Peter A.; Kürschner, Wolfram Michael & Bucher, Hugo
(2011).
Terrestrial ecosystems during and following the end-Permian mass extinction - or from spore spike to spore spike.
-
Schneebeli-Hermann, Elke; Kürschner, Wolfram Michael; Hochuli, Peter A.; Goudemand, Nicolas; Ware, David & Bucher, Hugo
[Vis alle 7 forfattere av denne artikkelen]
(2011).
Permian-Triassic palaeoenvironment inferred from palynofacies data of Amb, Salt Range, Pakistan.
-
Hincke, Alexandra J.C.; Kürschner, Wolfram Michael; Lotter, André F.; Tinner, Willy & Kaltenrieder, Petra
(2011).
Plants in a low CO2 world: validation of botanical proxies for the Pleistocene.
-
Hincke, Alexandra JC; Kürschner, Wolfram Michael; Lotter, André F.; Tinner, Willy & Kaltenrieder, Petra
(2011).
Plants in a low CO2 world: validation of botanical proxies for the Pleistocene.
-
Elkelani, Mohamed; Reichart, Gert Jan; Damsté, Jaap Sinninghe; Smeenk, Zwier; Kürschner, Wolfram Michael & Brinkhuis, Henk
[Vis alle 7 forfattere av denne artikkelen]
(2011).
Palaeoenvironmental change reflected by carbon isotopes and palynology in the Early Silurian of the Tanezzuft Formation, Libya.
-
Kürschner, Wolfram Michael
(2011).
Peculiarities of Permian – Triassic palynological records.
-
Kürschner, Wolfram Michael & Mueller, Steven
(2015).
Stratigraphy and depositional environments of the Boreal and Tethyan Early Carnian (Triassic) - Evidence by palynology and geochemistry.
Akademika forlag.
ISSN 1501-7710.
1664(1664).