Pedologic-biologic feedbacks on the Merced River chronosequence: The role of pocket gophers (Thomomys bottae) in Mima mound-vernal pool ecosystems of the San Joaquin Valley

Distinctive Mima mound topography, found on all continents except Antarctica, has long inspired intense interest, both because of the uncertainty surrounding its origin, as well as the rich biodiversity often found in the adjacent depressional vernal pool wetlands. Emerging from the array of explana...

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Bibliographic Details
Main Author: Reed, Sarah Elizabeth
Other Authors: Amundson, Ronald
Format: Other/Unknown Material
Language:English
Published: eScholarship, University of California 2013
Subjects:
Online Access:https://escholarship.org/uc/item/893376j7
id ftcdlib:oai:escholarship.org/ark:/13030/qt893376j7
record_format openpolar
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language English
topic Environmental science
Bioturbation
Geomorphology
Gopher
LIDAR
Mima mound
Spatial analysis
spellingShingle Environmental science
Bioturbation
Geomorphology
Gopher
LIDAR
Mima mound
Spatial analysis
Reed, Sarah Elizabeth
Pedologic-biologic feedbacks on the Merced River chronosequence: The role of pocket gophers (Thomomys bottae) in Mima mound-vernal pool ecosystems of the San Joaquin Valley
topic_facet Environmental science
Bioturbation
Geomorphology
Gopher
LIDAR
Mima mound
Spatial analysis
description Distinctive Mima mound topography, found on all continents except Antarctica, has long inspired intense interest, both because of the uncertainty surrounding its origin, as well as the rich biodiversity often found in the adjacent depressional vernal pool wetlands. Emerging from the array of explanations proposed, a biological mechanism for mound formation has steadily gained strength. According to this model, subterranean animals such as pocket gophers build the small hillocks as a response to changes in soil thickness and permeability caused by pedogenesis (soil formation). However, the precise mechanics of the hypothesis -- how soil weathering leads to changes in gopher soil movement and how the modified soil movement leads to the widespread Mima mound features -- are not understood. To address this issue, this thesis presents three related efforts to document and explain Mima mound morphology and to elucidate the linkages between soil formation processes, mound form and distribution, and biotic sediment transport. The research targets the effects of pedogenesis by focusing on a set of alluvial terraces in the San Joaquin Valley of California, a chronosequence which ranges in age from a few thousand to a few million years old. In the first portion of the study, I designed a custom algorithm which automatically identifies Mima mounds from LIDAR (light detection and ranging) data in order to analyze the morphology and spatial patterns of the microtopography across the soil age gradient. I demonstrate that mound size changes systematically with soil age and with depth to a restrictive layer, consistent with the predictions of the biologic model. Further, I show that the nearly quarter-million mounds in the study are distributed in a highly regular pattern, on scales consistent with the home range of pocket gophers, adding further support to the proposal that gophers created the topography. In the second part of this dissertation, I developed a method to use radio frequency identification tags (as a proxy for soil particles) and periodic aboveground mapping of gopher soil movement to quantify gopher sediment transport vectors on each chronosequence surface. I found that gophers on Mima mounds move soil uphill and towards the center of mounds, and I show that this moundward tendency increases with soil age and the environmental pressure caused by soil formation over long time periods. Third, I combined the morphometric measurements with the the sediment transport data from the first two parts of the study and developed a sediment transport model which estimates mound erosion and swale deposition rates. If the Mima mounds are steady-state landscape features, erosion must be balanced by a restorative upslope transport. I show that the erosion rates estimated for this study are largely counteracted by the observed rates of sediment mounding via pocket gopher burrowing, supporting the notion that bioturbation plays a dominant role in maintaining Mima mound terrain. Finally, I use LIDAR measurements and results from published gopher physiology research to develop a model that approximates the energy required for the formation of Mima mounds (shearing, pushing, and uplifting soil) and their maintenance (counteractions to erosion). This energy estimate was compared to estimates of energy available to gopher populations in the region. The results indicate that gophers have ample energy to build typical Mima mounds in as little as 100 years, thus strongly supporting a biotic mechanism of Mima mound development and maintenance.
author2 Amundson, Ronald
format Other/Unknown Material
author Reed, Sarah Elizabeth
author_facet Reed, Sarah Elizabeth
author_sort Reed, Sarah Elizabeth
title Pedologic-biologic feedbacks on the Merced River chronosequence: The role of pocket gophers (Thomomys bottae) in Mima mound-vernal pool ecosystems of the San Joaquin Valley
title_short Pedologic-biologic feedbacks on the Merced River chronosequence: The role of pocket gophers (Thomomys bottae) in Mima mound-vernal pool ecosystems of the San Joaquin Valley
title_full Pedologic-biologic feedbacks on the Merced River chronosequence: The role of pocket gophers (Thomomys bottae) in Mima mound-vernal pool ecosystems of the San Joaquin Valley
title_fullStr Pedologic-biologic feedbacks on the Merced River chronosequence: The role of pocket gophers (Thomomys bottae) in Mima mound-vernal pool ecosystems of the San Joaquin Valley
title_full_unstemmed Pedologic-biologic feedbacks on the Merced River chronosequence: The role of pocket gophers (Thomomys bottae) in Mima mound-vernal pool ecosystems of the San Joaquin Valley
title_sort pedologic-biologic feedbacks on the merced river chronosequence: the role of pocket gophers (thomomys bottae) in mima mound-vernal pool ecosystems of the san joaquin valley
publisher eScholarship, University of California
publishDate 2013
url https://escholarship.org/uc/item/893376j7
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation qt893376j7
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spelling ftcdlib:oai:escholarship.org/ark:/13030/qt893376j7 2023-05-15T13:58:20+02:00 Pedologic-biologic feedbacks on the Merced River chronosequence: The role of pocket gophers (Thomomys bottae) in Mima mound-vernal pool ecosystems of the San Joaquin Valley Reed, Sarah Elizabeth Amundson, Ronald 2013-01-01 application/pdf https://escholarship.org/uc/item/893376j7 en eng eScholarship, University of California qt893376j7 https://escholarship.org/uc/item/893376j7 public Environmental science Bioturbation Geomorphology Gopher LIDAR Mima mound Spatial analysis etd 2013 ftcdlib 2020-06-06T07:55:56Z Distinctive Mima mound topography, found on all continents except Antarctica, has long inspired intense interest, both because of the uncertainty surrounding its origin, as well as the rich biodiversity often found in the adjacent depressional vernal pool wetlands. Emerging from the array of explanations proposed, a biological mechanism for mound formation has steadily gained strength. According to this model, subterranean animals such as pocket gophers build the small hillocks as a response to changes in soil thickness and permeability caused by pedogenesis (soil formation). However, the precise mechanics of the hypothesis -- how soil weathering leads to changes in gopher soil movement and how the modified soil movement leads to the widespread Mima mound features -- are not understood. To address this issue, this thesis presents three related efforts to document and explain Mima mound morphology and to elucidate the linkages between soil formation processes, mound form and distribution, and biotic sediment transport. The research targets the effects of pedogenesis by focusing on a set of alluvial terraces in the San Joaquin Valley of California, a chronosequence which ranges in age from a few thousand to a few million years old. In the first portion of the study, I designed a custom algorithm which automatically identifies Mima mounds from LIDAR (light detection and ranging) data in order to analyze the morphology and spatial patterns of the microtopography across the soil age gradient. I demonstrate that mound size changes systematically with soil age and with depth to a restrictive layer, consistent with the predictions of the biologic model. Further, I show that the nearly quarter-million mounds in the study are distributed in a highly regular pattern, on scales consistent with the home range of pocket gophers, adding further support to the proposal that gophers created the topography. In the second part of this dissertation, I developed a method to use radio frequency identification tags (as a proxy for soil particles) and periodic aboveground mapping of gopher soil movement to quantify gopher sediment transport vectors on each chronosequence surface. I found that gophers on Mima mounds move soil uphill and towards the center of mounds, and I show that this moundward tendency increases with soil age and the environmental pressure caused by soil formation over long time periods. Third, I combined the morphometric measurements with the the sediment transport data from the first two parts of the study and developed a sediment transport model which estimates mound erosion and swale deposition rates. If the Mima mounds are steady-state landscape features, erosion must be balanced by a restorative upslope transport. I show that the erosion rates estimated for this study are largely counteracted by the observed rates of sediment mounding via pocket gopher burrowing, supporting the notion that bioturbation plays a dominant role in maintaining Mima mound terrain. Finally, I use LIDAR measurements and results from published gopher physiology research to develop a model that approximates the energy required for the formation of Mima mounds (shearing, pushing, and uplifting soil) and their maintenance (counteractions to erosion). This energy estimate was compared to estimates of energy available to gopher populations in the region. The results indicate that gophers have ample energy to build typical Mima mounds in as little as 100 years, thus strongly supporting a biotic mechanism of Mima mound development and maintenance. Other/Unknown Material Antarc* Antarctica University of California: eScholarship