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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What´s New on Links for Palaeobotanists?
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.
Marilyn Fox and Vicki Yarborough Fitzgerald:
A
Review of Vertebrate Fossil Support (and storage) Systems at the Yale Peabody
Museum of Natural History. Powerpoint presentation.
This expired link is still available through the Internet Archive´s
Wayback Machine.
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.
Department of Geological Sciences, University of Colorado, Boulder, CO:
Web-based instruction.
Annotated links to information on using the web to teach. Go to:
CzPaleobotany.
See especially: Cenozoic Elevation of the Rocky Mountains,
Paleobotanical
Methods. About fossil classification (nearest living relative, physiognomy and CLAMP) and
climate and elevation analysis.
These expired links are now available through the Internet Archive´s
Wayback Machine.
!
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. Trümper et al. (2023):
Decoding
the drivers of deep-time wetland biodiversity: insights from an early Permian tropical
lake ecosystem. Open access,
Palaeontology, doi: 10.1111/pala.12652.
Note figure 17: 1 7 . Reconstruction of the Manebach Lake ecosystem.
"... We reconstruct the trophic structure and age of the early Permian
Manebach Lake ecosystem, Germany
[...] The results indicate woody-debrisbearing lake littorals devoid of semi-aquatic and aquatic
plants as places suitable for stromatolites to grow,
underpin the model of declining freshwater-shark diversity in most
Permian Variscan basins, demonstrate fish/amphibian ratios
in limnic assemblages ..."
M. Haworth and J. McElwain (2008): Hot, dry, wet, cold or toxic? Revisiting the ecological significance of leaf and cuticular micromorphology. In PDF, Palaeogeography, Palaeoclimatology, Palaeoecology, 262: 79–90. See also here.
L.I. Anderson and M. Taylor (2008):
Charles
W. Peach,
Palaeobotany and Scotland (in PDF). The Geological Curator, 8: 393-425.
Thin sections of Devonian plants!
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.
!
D. Chakrabarty (2018):
Anthropocene time. Open access,
History and Theory, 57: 5-32.
"... this article proceeds to discuss
the differences between human-historical time and the time of geology as they relate to the
concept of the Anthropocene ..."
J.E. Francis (1983):
The
dominant conifer of the Jurassic Purbeck formation, England.In PDF,
Palaeontology, 26.
Note figure 3: Reconstruction of the dominant Purbeck conifer.
This expired link is still available through the Internet Archive´s Wayback Machine.
University of California Museum of Paleontology, Berkeley (with support provided by the National Science Foundation and the
Howard Hughes Medical Institute):
Understanding Evolution.
Understanding Evolution is a non-commercial, education website, teaching the science and
history of evolutionary biology. Go to:
History
of life on Earth.
Topics are "From soup to cells - The origin of life", "Evolution and the fossil record",
"Deep Time" (an interactive timeline), etc.
Still available through the Internet Archive´s
Wayback Machine.
D.M. Jarzen, Florida Museum of Natural History:
Paleobotany
Collection Policies.
Website saved by the Internet Archive´s Wayback Machine.
J. Zalasiewicz et al. (2013): Chronostratigraphy and geochronology: A proposed realignment. In PDF, GSA Today, 23.
John Horgan, Scientific American:
Life, Life Everywhere.
This expired link is still available through the Internet Archive´s Wayback Machine.
! 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.
M.J. Tyler et al. (2023):
Calamities
causing loss of museum collections: a historical and global perspective
on museum disasters. In PDF,
Zootaxa, 5230: 153–178. https://doi.org/10.11646/zootaxa.5230.2.2.
Note here
as well.
"... We review the loss or damage of museum collections globally
[...] The significance of the loss of type material would be ameliorated if,
when there are numerous paratypes or
syntypes, members of a type series were distributed among
several institutions. This is currently common practice but
historically this was not always the case and might not be
possible if only a single holotype is available ..."
Michael A. Kruge, Dept. of Geology
Southern Illinois Univ., Carbondale, IL:
Chemistry
Of Fossil Charcoal In Cretaceous-Tertiary Boundary Strata,
Arroyo El Mimbral, Mexico.
The link is to a version archived by the Internet Archive´s Wayback Machine.
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 ..."
!
A.M. Gurnell and W. Bertoldi (2024):
Plants
and river morphodynamics: the emergence of fluvial biogeomorphology. Open access,
River Research and Applications, 40: 875-1150.
"... we present an annotated bibliographic
overview of the development of fluvial biogeomorphology, whereby the text describes
broad trends but is supported by tables of citations that can deliver greater detail ..."
! 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 ..."
D.G. Miralles et al. (2025):
Vegetation–climate
feedbacks across scales. Open access,
Annals of the New York Academy of Sciences, 1544.
Note figure 2: Interaction between vegetation and climate trends and extremes.
"... Our goal is to highlight the state of science and review recent studies that
may help advance our collective understanding of vegetation feedbacks and the role
they play in climate ..."
!
G.E. Mustoe (2025):
Mineralization
of Fossil Wood with Macrocrystalline Quartz: A Microscopic Investigation. Open access,
Minerals, 15. https://doi.org/10.3390/min15030225.
"... there are only a few principal requirements.
Dissolved Si concentration need to be at saturation level, and pH, Eh, and temperature
parameters must be suitable for silica precipitation. The precipitation rate must be slow
enough to allow the development of the well-ordered lattices necessary for the growth of
quartz crystals. Macroscopic crystal growth requires sufficient open space for the formation
of individual terminated shapes. These spaces can be related to anatomical features (e.g.,
vessels in angiosperm wood) or structural defects (e.g., fractures or rot pockets). When
wood petrifaction has occurred in series of episodes ..."
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