An annotated collection of pointers
to information on palaeobotany
or to WWW resources which may be of use to palaeobotanists
(with an Upper Triassic bias).
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Z. Xu et al. (2025):
Normalization
of fossil plant megafossil databases for diversity and
palaeobiogeography analyses by filtering taxonomic duplication:
Principles, methods, examples, and recommendations. Open access,
Palaeogeography, Palaeoclimatology, Palaeoecology, 678. See likewise
here
(in PDF).
Note figure 1: World palaeogeography from the late Permian to Middle Triassic.
Figure 3: Representative world palaeogeography maps showing locations of coal ball floras.
Figure 5: Total, extinction and origination taxon number from the middle Permian
to Late Triassic floras of South China.
"... We use two case studies to highlight the impact of normalization
by analysing raw (unfiltered) versus normalized (filtered) data ..."
!
F. Westall and S. Xiao (2024):
Precambrian
Earth: Co-evolution of life and geodynamics. Free access,
Precambrian Research, 414.
!
Note figure 1: Evolution of Earth’s atmosphere through time.
Figure 4: Microbially induced sedimentary structures.
Melanie DeVore, Georgia College and State University,
Milledgeville, GA:
Life
of the PreCambrian: Archean & Proterozoic.
!
Plant
Origin and Evolution.
Powerpoint presentations. Provided by
D. Freile, New Jersey City University:
Historical
Geology.
These expired links are still available through the Internet Archive´s Wayback Machine.
L.M. Alves, Manhattan College, and
P.A. Grove, College of Mount Saint Vincent:
Teaching
Introductory Biology.
Go to:
Rich
Sources of Links for Introductory Biology.
Still available through the Internet Archive´s
Wayback Machine.
Charles H. Smith (Library Public Services,
Western Kentucky University, Bowling Green),
Joshua Woleben, and Carubie Rodgers:
Some Biogeographers,
Evolutionists and Ecologists:
Chrono-Biographical Sketches. Go to:
Listing
by Discipline.
Scroll down to "paleobotany", or "botany" (including palaeobotany).
Websites outdated. Links lead to versions archived by the Internet Archive´s Wayback Machine.
!
M. Laaß et al. (2025):
Host-specific
leaf-mining behaviour of holometabolous insect larvae in the early Permian. Open access,
Scientific reports, 15. doi.org/10.1038/s41598-025-15413-x. See here
as well.
Note figure 5: Co-occurrence of endophytic oviposition and Asteronomus maeandriformis in
Autunia conferta.
"... We re-examined the controversial feeding trace of Asteronomus maeandriformis
[...] Our results unequivocally show that
endophytic feeding behaviour evolved in the holometabolan clade at least by the earliest Permian
and, therefore, more than 40 Ma earlier than hypothesised. The findings reveal complex organism
interactions in late Palaeozoic ecosystems ..."
R.R. Schoch and D. Seegis (2014):
Taphonomy,
deposition and pedogenesis
in the Upper Triassic dinosaur beds of
Trossingen. In PDF.
Palaeobiodiversity and
Palaeoenvironments.
"... Seasonal wetting and drying leads
to frequent expansion and shrinkage of the soil material,
resulting in an extensive amalgamation (peloturbation) ..."
Spektrum.de :
Peloturbation
(in German).
Wikipedia, the free encyclopedia:
Category:Pedology.
Category:Types of soil.
!
Vertisol.
S. Mazrou and A. Boutaleb (2025):
Reply
to “Comment on: Depositional palaeoenvironments in a tide-influenced delta plain with amphibian
and Cycadophyta remains – the Triassic Zarzaitine Formation (Algerian eastern Sahara) by S.
Mazrou, Y. Lasnami, J. Amer, A. Boutaleb: Geologos 30, 3 (2024): 209–229“. Free access,
Geologos, 31: 83–93. https://doi.org/10.14746/logos.2025.31.1.07.
"... We shall illustrate below that no information, detail or anything else was presented by
Dahoumane et al. concerning the Triassic terrain studied, except for a plate presenting
photographs, interpretations of which are all erroneous. We would have appreciated academic
critique that could have helped us improve our work, instead of wasting our time
responding to false allegations and nonsensical comments ..."
S. Mazrou et al. (2024):
Depositional
palaeoenvironments in a tide-influenced delta plain with amphibian and
Cycadophyta remains – the Triassic Zarzaitine Formation
(Algerian eastern Sahara). In PDF,
Geologos, 30: 209–229. https://doi.org/10.14746/logos.2024.30.3.19. See here
as well.
Note figure 12: Trees in situ within sandstone channel infill.
A. Dahoumane et al. (2025):
Comment
on “Depositional palaeoenvironments in a tide-influenced delta plain with amphibian and
Cycadophyta remains – the Triassic Zarzaitine Formation (Algerian eastern Sahara)” S. Mazrou,
Y. Lasnami, J. Amer, A. Boutaleb (2024): Geologos 30, 3 (2024): 209–229“. Free access,
Geologos, 31: 73–81. https://doi.org/10.14746/logos.2025.31.1.06.
"... Mazrou et al. (2024) fail to integrate previous findings and do not position their work within
a scientific continuum. Their study is marked by methodological shortcomings, weakly supported
interpretations, and fundamental errors in palaeontology, ichnology and facies analysis ..."
V. Robin and O. Nelle (2011): Main data and general insights of recent soil charcoal investigations on nine sites in Central Europe. In PDF, SAGVNTVM Extra.
Geologos.
The Journal of Adam Mickiewicz University, Poland.
Sophia Kossida, Principles of Protein Structure Using the Internet:
Molecular
Phylogenetics.
Still available via Internet Archive Wayback Machine.
Q. Fu et al. (2024):
Unique
Jurassic ovaries shed a new light on the nature of carpels. Open access,
Plants, 13. https://doi.org/10.3390/plants13162239.
"... A recently raised hypothesis stated
that a carpel is a composite organ derived from an ovule-bearing axis and a subtending and
enclosing leaf
[...] we report a new fruit/ovary, Xenofructus dabuensis gen. et sp. nov, from the Middle
Jurassic of Liaoning, China. Surprisingly, these Jurassic ovaries clearly demonstrate the
existence of free central placentation in early angiosperms. It appears that this new fossil
provides a new insight into the evolution of placentation in angiosperms ..."
Gar W. Rothwell, Department of Environmental and Plant Biology, Ohio University, Athens:
Angiophytes: Using Whole Plant Concepts to Interpret Angiosperm Origins.
Selected
Literature.
Selected
Examples.
Images and reconstructions of
Archaeanthus, Caloda reynoldsii, Joffrea speirsii, Polyptera manningii,
Limnobiophyllum scutatum, Macginitea, Eorhiza/Princetonia.
Links archived by the Internet Archive´s Wayback Machine.
S. Sarkar et al. (2024): Palynology and palynofacies analysis of the Subathu Formation (Early Ypresian-Middle Lutetian) of Morni Hills, Haryana, India. In PDF, Journal of Palaeosciences, 73: 2583–4266.
C.A. Jaramillo and F.E. Oboh-Ikuenobe (1999):
Sequence
stratigraphic interpretations from palynofacies, dinocyst and lithological data of
Upper Eocene-Lower Oligocene strata in southern Mississippi and Alabama, U.S. Gulf Coast.
PDF file, Palaeogeography, Palaeoclimatology, Palaeoecology, 145: 259-302.
Still available through the Internet Archive´s
Wayback Machine.
Anna-Lena Anderberg, Department of Palaeobotany,
Swedish Museum of Natural History, Stockholm:
Rhaetian
and Jurassic plants of Scania.
This database includes the Rhaetian and Jurassic plant fossils from Scania, southern Sweden,
housed in the Stockholm collections.
Still available via Internet Archive Wayback Machine.
University of Oregon Eugene, OR.
! Electron
Probe Micro Analysis Course Materials.
This course (for Mineralogy, Petrology and Materials Science) is a laboratory
course covering the theory and application of EPMA (electron probe micro analysis) and
SEM (scanning electron microscopy) as an integrated and multi-disciplinary subject
covering aspects of physics, chemistry, geology and statistics plus practical hands-on
experience with the instruments themselves. See for example:
1
Introduction to the EPMA/SEM laboratory: An introduction to the technique followed by a short
tour of the facilities, including discussion of lecture notes and suggested reading materials.
10
Statistics: The essential key to scientific analysis.
13 Digital
Imaging (Lecture and Lab): Imaging and mapping:
An overview of electron and x-ray imaging and mapping techniques.
Lecture notes, Powerpoint presentations.
S.P. Xie et al. (2009):
Altitudinal
variation in Ginkgo leaf characters: Clues to paleoelevation reconstruction.
PDF file, Science in China Series D: Earth Sciences, 52: 2040-2046. See likewise
here.
"... The results show that leaf area, petiole length, and stomatal parameters have no obvious
linear relationship with altitude (...). The results also suggest that the
differences in stomatal density and stomatal index between sun and shade leaves had more influence
on paleoelevation reconstruction than that in other parameters ..."
A. Roth-Nebelsick (2007):
Computer-based
Studies of Diffusion through Stomata of Different Architecture. PDF file,
Ann. Bot., 100: 23-32. See also
here.
Recovered from the Internet Archive´s
Wayback Machine.
N. Gentis et al. (2024): First fossil woods and palm stems from the mid-Paleocene of Myanmar and implications for biogeography and wood anatomy. Open access, American Journal of Botany, 111.
C.T. Gee and M.M. Howell (2024): International Workshop on Fossilization. In PDF, Terra Nostra, DFG Research Unit FOR 2685 at the University of Bonn, Germany June 14-17, 2024.
T. Mesaglio et al. (2025): Citizen science records are fuelling exciting discoveries of new plant species. Open access, American Journal of Botany, 112.
!
G. Jovanovski et al. (2023):
Chemistry
and geology of coal: nature, composition, coking,
gasification, liquefaction, production of chemicals, formation,
peatification, coalification, coal types, and ranks. In PDF
ChemTexts, 9.
See likewise
here.
!
Note figure 13: Scheme of formation of different coal types.
!
Table 4: US coal rank system showing the parameters used to define ranks.
American Journal of Botany.
The American Journal of Botany (AJB),
published by the Botanical Society, is the Society’s flagship research journal.
Anais
da Academia Brasileira de Ciências.
Annals of the Brazilian Academy of Sciences.
See here
as well.
F. Battista and C.L. Schultz (2024):
Sampling
and collector biases as taphonomic filters: an overview. Open access,
Anais da Academia Brasileira de Ciências, 96.
https://doi.org/10.1590/0001-3765202420231242. See also
here
(in PDF).
Note figure 1: Conceptual map of the factors determining biases in the fossil
record and palaeontological collections.
Figure 2: Conceptual map of further anthropogenic biases that lead to
the loss, even definitive, of taphonomic information and consequent biased results.
L.A. Vietti et al. (2015):
Rapid
formation of framboidal sulfides on bone surfaces from a simulated marine carcass-fall. In PDF,
Palaios, 30: 327–334.
See likewise
here.
!
C.C. Loron et al. (2025):
Prototaxites
was an extinct lineage of multicellular terrestrial eukaryotes
bioRxiv, https://doi.org/10.1101/2025.03.14.643340.
"... We report that Prototaxites taiti was the largest organism in the Rhynie ecosystem
and its anatomy was fundamentally distinct from all known extant or extinct fungi. Furthermore,
our molecular composition analysis indicates that cell walls of P. taiti include aliphatic,
aromatic, and phenolic components most similar to fossilisation products of lignin, but no
fossilisation products characteristic of chitin or chitosan, which are diagnostic of all
groups of extant and extinct fungi
[...] Prototaxites was not a fungus ..."
S.G. Razafimandimbison et al. (2025): Phylogeny and divergence times of the African and Malagasy Podocarpus (Podocarpaceae) and their taxonomic and biogeographic implications. Open access, Taxon. https://doi.org/10.1002/tax.70023.
! J.E.A. Marshall et al. (2025):
Terrestrial
palaeoclimate, mercury, atmospheric CO2 and land plants through the Late Devonian
mass extinction. Free access,
Journal of the Geological Society, 182.
"... a highly expanded terrestrial section from East Greenland is
reported, which includes records of palaeoenvironment, palaeoclimate, carbon isotopes
from plant debris, sedimentary mercury and plant spores
[...] The Heintzbjerg section is the first record from a terrestrial
F-F [Frasnian–Famennian] Late Devonian mass extinction ..."
C.J. Cleal et al. (2024): Early coal swamp vegetation from the Serpukhovian lower Clackmannan Group of Scotland. Free access, Fossil Imprint, 80: 35–67.
P.E. Jardine et al. (2025):
Which
morphological traits can be used to reconstruct genome size in fossil plants? Assessing
sporomorph size and stomatal guard cell length as paleo-genome size proxies. Open access,
Paleobiology, 51: 378–391.
"... We show that sporomorph size has a complicated but
mostly weak relationship with genome size, suggesting that it is a poor proxy to use in the fossil
record. Stomatal guard cell length has a much stronger relationship with genome size, with the
potential to provide accurate genome size estimates ..."
! L. Liu et al. (2025):
Ordovician
marine Charophyceae and insights into land plant derivations. In PDF,
Nature Plants. https://doi.org/10.1038/s41477-025-02003-y.
See here
as well.
Note figure 4: Morphological and palaeoecological reconstructions of Tarimochara
miraclensis gen. et sp. nov.
Figure 6: Outline of the early Palaeozoic record of streptophyte algae
and embryophytes.
"... This discovery demonstrates that at least some species of Charophyceae
inhabited shallow normal marine environments at that time. Moreover,
these early Charophyceae show that some key morphological innovations
associated with an evolutionary transition between streptophyte algae
and land plants had occurred before the early Katian ..."
J.S. Ferraz et al. (2025):
An
oasis in Western Gondwana: A diverse Guadalupian paleoflora from South America. In PDF,
Journal of South American Earth Sciences, 158.
See here
as well.
Note figure 9: Paleoenvironmental reconstruction of the Cerro Chato outcrop.
M. Krings (2025):
Oldest
fossil evidence of cell wall apposition as a plant defense
response to fungal invasion, with notes on an analogous mechanism
in equally old arbuscular mycorrhizal fungi. Abstract, in PDF.
N. Jb. Geol. Paläont. Abh., 315: 175–185. See
here as well.
Rhynia gwynne-vaughanii, a small land plant
sporophyte from the Lower Devonian Rhynie chert, show preserved
papilla-like cell wall appositions encasing invasive fungal hyphae
[...] some early land plants were evidently able to
recognize invasive fungi and respond to their presence by remodeling
and reinforcing the cell walls specifically at the sites of attempted invasion ..."
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