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The geomorphic work of the European mole (Talpa europaea): long-term monitoring of molehills using structure-from-motion photogrammetry

Abstract:

Moles—small insectivorous mammals of the family Talpidae—are widespread across the Northern Hemisphere. These subterranean mammals are easily detected through the mounds, or molehills, they construct as surface bioproducts of tunnel systems excavated underground. The dense aggregation of these bioconstructions in a range of environments (e.g. floodplains, woodland, coastal dunes, upland regions, etc.) indicates that moles may play an important role in sediment systems. However, compared to other fossorial mammals (e.g. gophers, rabbits) the impact of moles as direct and indirect biogeomorphic agents is poorly understood. Furthermore, little is known about how molehills develop and degrade over time, or how long they persist as landscape features.

By examining molehills created by the European mole (Talpa europaea) over four months on a floodplain in Oxfordshire, UK, we provide a quantitative assessment of how these landforms evolve over time and space. Through the creation of high-resolution digital elevation models (DEMs) using structure-from-motion (SfM) photogrammetry, we derive a variety of metrics describing molehill morphology and produce a detailed record of how molehills change at weekly time intervals. In addition, measurements of molehill volume are used to estimate the excavation rate of moles over a month. Findings show that (i) molehills are dynamic landforms that change in size and shape in response to phases of construction, collapse, erosion, and rebuilding, (ii) rates of degradation are influenced by soil characteristics and seasonal weather conditions, (iii) molehills can persist as landscape features for several months, (iv) and moles are capable of moving a substantial volume of sediment in highly active areas (3.89 m3 ha-1 month-1). Future work is now needed to determine the geomorphic impact of T. europaea over larger spatial scales (e.g. river catchments) and longer timescales (e.g. years‒decades) to determine its importance in relation to other bioturbators and within the wider sediment system.

Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1002/esp.6008

Authors

More by this author
Institution:
University of Oxford
Division:
SSD
Department:
SOGE
Sub department:
Geography
Role:
Author
ORCID:
0000-0002-7915-2968
More by this author
Institution:
University of Oxford
Division:
SSD
Department:
SOGE
Sub department:
Geography
Role:
Author


Publisher:
Wiley
Journal:
Earth Surface Processes and Landforms More from this journal
Volume:
49
Issue:
15
Pages:
4991-5011
Publication date:
2024-10-13
Acceptance date:
2024-09-27
DOI:
EISSN:
1096-9837
ISSN:
0197-9337


Language:
English
Keywords:
Pubs id:
2035816
Local pid:
pubs:2035816
Deposit date:
2024-10-02
ARK identifier:

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