Ahmed, S.E., and Cain, R.F.
Revisions of the genera Sporormia and Sporormiella
. Canadian Journal of Botany
50, (1972). 419–477.
Aptroot, A., and van Geel, B.
Fungi of the colon of the Yukagir mammoth and from stratigraphically related permafrost samples. Review of Paleobotany and Palynology
141, (2006). 225–230.
Barnosky, A.D., Koch, P.L., Feranec, R.S., Wing, S.L., and Shabel, A.B.
Assessing the causes of late Pleistocene extinction on the continents. Science
306, (2004). 70–75.
Blackford, J.J., and Innes, J.B.
Linking current environments and processes to fungal spore assemblages: surface NPM data from woodland environments. Review of Paleobotany and Palynology
141, (2006). 179–187.
Brenner, M., and Binford, M.W.
Relationships between concentrations of sedimentary variables and trophic state in Florida lakes. Canadian Journal of Fisheries and Aquatic Science
45, (1988). 294–300.
Burney, D.A., Robinson, G.S., and Burney, L.P.
Sporormiella and the late Holocene extinctions in Madagascar. Proceedings of the National Academy of Sciences
100, (2003). 10800–10805.
Spores of the dung fungus Sporormiella: increased abundances in historic sediments and before Pleistocene megafaunal extinctions. Quaternary Research
28, (1987). 290–294.
Davis, O.K., and Moratto, M.F.
Evidence for a warm-dry early Holocene in the Western Sierra: pollen and plant macrofossil analysis of Dinkey and Exchequer Meadows. Madroño
35, (1988). 128–145.
Davis, O.K., Shafer, D., (2002).
Sporormiella fungal spores, a palynological means of detecting herbivore density. Proceedings of the “Faeces Facies Symposium.�.�.
Davis, O.K., and Shafer, D.
Sporormiella fungal spores, a palynological means of detecting herbivore density. Palaeogeography, Palaeoclimatology, Palaeoecology
237, (2006). 40–50.
Davis, O.K., Kolva, D.A., and Mehringer, P.J.
Pollen analysis of Wildcat Lake, Whitman County, Washington: the last 100 years. Northwest Science
51, (1977). 13–30.
Davis, O.K., Agenbroad, L., Martin, P.S., and Mead, J.I.
The Pleistocene dung blanket of Bechan Cave, Utah. Special Publication of the Carnegie Museum of Natural History
8, (1984). 267–282.
Davis, O.K., Heavly, R.H., and Foust, R.D.
A comparison of historic and prehistoric vegetation change caused by man in Central Arizona. Assoication of Stratigraphic Palynologists Contribution Series
16, (1985). 63–76.
Ebersohn, C., and Eicker, A.
Determination of the coprophilous fungal fruit body successional phase and the delimitation of species association classes on dung substrates of African game animals. Botanical Bulletin Academy of Science
38, (1997). 183–190.
Faegri, K., and Iverson, J.
Textbook of Pollen Analysis. 4th Edition (1989). John Wiley & Sons, Chicester (England). 328
Graf, M., and Chmura, G.
Development of modern analogues for natural, mowed, and grazed grasslands using pollen assemblages and coprophilous fungi. Review of Paleobotany and Palynology
141, (2006). 139–149.
Late Pleistocene mammalian extinctions in North America: taxonomy, chronology, and explanations. Journal of World Prehistory
5, (1991). 193–231.
Gu, B., Schelske, C.L., and Brenner, M.
Relationship between diment and plankton isotope ratios (d13C and d15N) and primary productivity in Florida Lakes. Canadian Journal of Fisheries and Aquatic Science (1996).
Prehistoric overkill. Martin, P.S., and Wright, H.E.
Pleistocene Extinctions: The Search for a Cause. (1967). Yale University Press, New Haven, CT. 75–120.
Martin, P.S., and Stuart, A.J.
Mammoth extinction: two continents and Wrangel Island. Radiocarbon
37, (1995). 7–10.
Pirozynski, K.A., Carter, A., and Day, R.G.
Fungal remains in Pleistocene ground squirrel dung from Yukon Territory, Canada. Quaternary Research
22, (1984). 375–382.
Diversity and occurrence of coprophilous fungi. Mycology Research
105, (2001). 387–402.
Robinson, G., Burney, L.P., and Burney, D.A.
Landscape paleoecology and megafaunal extinction in southeastern New York State. Ecological Monographs
75, (2005). 295–315.
Tablets with spores used in absolute pollen analysis. Pollen Spores
13, (1971). 615–621.
Váňová, M., and Kubátová, A.
Dung microcosms as another source of fungal biodiversity on areas with industrial deposits. Stránka
9, (2005). 121–131.
A late Pleistocene–Holocene pollen record of vegetation change from Little Willow Lake, Lassen Volcanic National Park, California. Conference Proceedings: PACLIM (2003). 65–80.