Buynevich,
I. V. 2023. Neoichnology of vertebrate traces along the western barrier coast
of Ukraine: preservation potential and subsurface visualization.Geo&Bio,
24: 99–105. [In English, with Ukrainian
summary]
Neoichnology of vertebrate traces along the western barrier
coast of Ukraine: preservation potential and subsurface visualization
A
diverse quite of vertebrate traces covers beach, aeolian, and bay-side
(deflation flats) surfaces along the NW Black Sea coast of Ukraine. These
include avian, ungulate, and canid footprints, as well as mammal burrows
(length >5 cm; depth ~2 cm). The preservation of biogenic structures is
enhanced by rapid burial (low-energy sedimentation or event deposition), algal
mat formation, and salt encrustation. Continuous high-frequency (800 MHz) ground-penetrating radar (GPR) imaging aided in visualizing
subsurface sections of an active burrow complex within a beach-dune ridge.
Images near an active fox burrow captured distinct subsurface anomalies
(point-source hyperbolic diffractions) in the upper aeolian section above the
water table. Unfilled tunnel sections are easily distinguished from buried
roots and other targets based on signal velocity and polarity reversals
relative to air-to-sediment response at the ground surface. The diffraction
geometry (angle) is related to signal velocity, providing valuable information
about relative saturation of the overlying substrate. Decimeter-scale
deformation of shallow reflections may be attributed to tracking surfaces, with
similar examples found immediately below modern surfaces affected by
anthropogenic trampling. It is likely that muddy lagoonal tracking surfaces may
be preserved under layers of sand (overwash or aeolian deposition) and,
following saltwater expulsion, may be recognized in geophysical images as clear
deformed paleo-surfaces. Heavy-mineral concentrations (e.g. magnetite-rich
sand) are common for beach and dune horizons that have undergone reworking and
such anomalies often accentuate physical and biogenic deformation structures.
Due to moderate-to-high fraction of ferri- and paramagnetic minerals, these
anomalies are also well-expressed in GPR images due to its electromagnetic
signal response. A conceptual framework of trace preservation potential
(taphonomy) and geophysical recognition (GPR) suitability is proposed for this
coastal region, with implications to paleo-environmental reconstruction.
Ilya V. Buynevich; Department of Earth and Environmental
Science, Temple University; 1901 N 13th Street, Philadelphia
19122, USA;
Email: coast@temple.edu; orcid: 0000-0002-3840-0208
Article info
Submitted:
23.03.2023. Accepted: 30.06.2023
References
Allen, J. R. L. 1989. Fossil vertebrate tracks and
indenter mechanics. Journal of the
Geological Society, London, 146:
600–602. https://doi.org/10.1144/gsjgs.146.4.0600
Allen, J. R. L. 1997. Subfossil mammalian tracks
(Flandrian) in the Severn Estuary, S.W. Britain: mechanics of formation, preservation
and distribution. Philosophical
Transactions of the Royal Society of London, B 352: 481–518. https://doi.org/10.1098/rstb.1997.0035
Buynevich, I. V., J. S. Darrow, Z. T. A.
Grimes, C. T. Seminack, N. Griffis. 2011. Ungulate tracks in coastal sands:
recognition and sedimentological significance. Journal of Coastal Research, SI 64: 334–338.
Buynevich, I.
V., H. A. Curran, L. A. Wiest, A. P. K. Bentley, S. V. Kadurin. [et al.]. 2014.
Near-surface imaging (GPR) of biogenic
structures in siliciclastic, carbonate, and gypsum dunes. In: Hembree, D. I., B. F. Platt, J. J. Smith
(eds). Experimental Approaches to
Understanding Fossil Organisms:Lessons from the Living. Springer, Dordrecht, the Netherlands, 405–418. https://doi.org/10.1007/978-94-017-8721-5_17
Buynevich, I. V.
2015. Recent vertebrate tracks in sandy substrates and their
paleoenvironmental implications: examples
from coastal Lithuania. Baltica, 28: 29–40. https://doi.org/10.5200/baltica.2015.28.04
Buynevich, I. V.
2020. Detection of
mineralogically accentuated biogenic structures with high-resolution geophysics:
implications for ichnology and geoecology. Journal of Geology, Geography and
Geoecology, 29: 252–257. https://doi.org/10.15421/112023
Chlaib, H. K., H. Mahdi, H. Al-Shukri, M.M. Su, A. Catakli,
N. Abd. 2014. Using ground penetrating radar in levee assessment to detect
small-scale animal burrows. Journal of
Applied Geophysics, 103:
121–131. https://doi.org/10.1016/j.jappgeo.2014.01.011
Fanelli, F., M. R. Palombo, G. L. Pillola, A. Ibba. 2007.
Tracks and trackways of “Praemegaceros”
cazioti (Depéret, 1897) (Artiodactyla, Cervidae) in Pleistocene coastal
deposits from Sardinia (Western Mediterranean, Italy). Bollettino della SocietàPaleontologica Italiana, 46: 47–54.
Fornós, J. J., R. G. Bromley, L. A.
Clemmensen, A. Rodriguez-Perea. 2002. Tracks and trackways of Myotragus
balearicus Bate (Artiodactyla, Caprinae) in Pleistocene aeolianites from Mallorca
(Balearic Islands, Western Mediterranean). Palaeogeography,
Palaeoclimatology, Palaeoecology, 180:
277–313. https://doi.org/10.1016/S0031-0182(01)00431-X
Frey, R. W., S. G. Pemberton,
1986. Vertebrate Lebensspuren in intertidal and supratidal environments,
Holocene barrier islands, Georgia: Senckenbergiana Maritima, 18: 45–99.
Hasiotis, S. T., B. F. Platt, D. I.
Hembree, M. Everhart. 2007. The trace-fossil record of vertebrates. In: Miller, W., III (ed.) Trace Fossils-Concepts, Problems, Prospects.
Elsevier Press, 196–218. https://doi.org/10.1016/B978-044452949-7/50138-8
Laporte, L. F., A. K. Behrensmeyer, 1980.
Tracks and substrate reworking by terrestrial vertebrates in Quaternary
sediments of Kenya. Journal of Sedimentary
Petrology, 50: 1337–1346. https://doi.org/10.1306/212F7BE9-2B24-11D7-8648000102C1865D
Loope, D. B. 1986. Recognizing and
utilizing vertebrate tracks in cross section, Cenozoic hoofprints from Nebraska.
Palaios,1: 141–151. https://doi.org/10.2307/3514507
Marty, D., A. Strasser, C. A. Meyer. 2009.
Formation and taphonomy of human
footprints in microbial mats of present-day tidal-flat environments:
implications for the study of fossil footprints. Ichnos, 16: 127–142.https://doi.org/10.1080/10420940802471027
Milàn, J., R. G. Bromley. 2006. True tracks, undertracks and eroded
tracks: experimental work with tetrapod tracks in laboratory and field. Palaeogeography, Palaeoclimatology,
Palaeoecology, 231: 253–264.
Milàn, J., L. B. Clemmensen, B. Buchardt,
N. Noe-Nygaar. 2007. A late Holocene tracksite in the Lodbjerg dune system,
northwest Jylland, Denmark. In: Lucas,
S. G., J. A. Spielman, M. Lockley. (eds). Cenozoic
vertebrate tracks and traces, vol. 42. New Mexico Museum of Natural History
and Science, Albuquerque, 241–250. https://doi.org/10.1016/j.palaeo.2004.12.022
Scott, J. J., R. W. Renaut, R. B. Owen.
2008. Preservation and paleoenvironmental significance of a footprinted surface
on the Sandai Plain, Lake Bogoria, Kenya Rift Valley. Ichnos, 15: 208–231. https://doi.org/10.1080/10420940802470573
Stott, P. 1996. Ground-penetrating radar:
a technique for investigating the burrow structure of fossorial vertebrates. Wildlife Research, 22: 519–530. https://doi.org/10.1071/WR9960519
Urban, T. M., M. R. Bennett, D. Bustos, S. W. Manning,
S. C. Reynolds, [et al.]. 2019. 3-D radar imaging unlocks the untapped
behavioral and biomechanical archive of Pleistocene ghost tracks. Scientific
Reports, 9: 16470. https://doi.org/10.1038/s41598-019-52996-8