DSpace Repository

Vegetational zonation in a swamp forest, Middle Pennsylvanian, Illinois Basin, U.S.A., indicates niche differentiation in a wetland plant community

Show simple item record

dc.contributor.author DiMichele, William A. en
dc.contributor.author Elrick, Scott D. en
dc.contributor.author Nelson, W. John en
dc.date.accessioned 2017-08-23T09:01:18Z
dc.date.available 2017-08-23T09:01:18Z
dc.date.issued 2017
dc.identifier.citation DiMichele, William A., Elrick, Scott D., and Nelson, W. John. 2017. "<a href="https%3A%2F%2Frepository.si.edu%2Fhandle%2F10088%2F32947">Vegetational zonation in a swamp forest, Middle Pennsylvanian, Illinois Basin, U.S.A., indicates niche differentiation in a wetland plant community</a>." <em>Palaeogeography palaeoclimatology palaeoecology</em>. 487:71&ndash;92. <a href="https://doi.org/10.1016/j.palaeo.2017.08.020">https://doi.org/10.1016/j.palaeo.2017.08.020</a> en
dc.identifier.issn 0031-0182
dc.identifier.uri https://hdl.handle.net/10088/32947
dc.description.abstract A rich fossil flora occurs in the roof shale of the Middle Pennsylvanian (Moscovian) age, Springfield Coal flanking the Galatia channel, a river deposit approximately 1 km in width and 150 km long, partially contemporaneous with the Springfield peat swamp. Siltstone and sandstone, &gt; 30 m thick, were deposited in the channel during the final estuarine phase. The river formed under seasonal subhumid climate during early deglaciation as marine waters retreated from the land surface. It existed continuously through glacial maximum, under increasingly humid climate, as a low-sediment or black-water river with peat along its flanks. During early deglaciation, under subhumid climate and sea-level rise, the river became a sediment-laden estuary, drowning the peat swamp and burying vegetation in place under extensive mudflats. This buried flora was studied in three underground mines in southern Illinois, permitting vegetation to be characterized spatially. Three transects, comprising 100 sites, a total linear distance of ~ 12 km, reveal distinct zonation perpendicular to the channel margin. An innermost belt, 0.5 to 2.5 km wide, consists almost exclusively of the pteridosperm Neuropteris flexuosa. North of a river bend, three belts succeed the N. flexuosa zone: mixed pteridosperms and marattialean tree ferns; mixed arborescent lycopsids and marattialians; lycopsids with rare marattialians. South and inside the same bend, N. flexuosa is succeeded by mixed lycopsids, particularly Sigillaria, and marattialean ferns. Within the transects, marattialian ferns have wider distribution than other groups, suggesting broader environmental tolerances. Neuropteris flexuosa channel-margin mono-dominance may reflect high sedimentation rates, elevated nutrient conditions, or floating-seed dispersal. Lycopsid dominance in interior areas conforms with tolerance of deep, standing water. The spatial scale examined affects our perception of community assembly. Overall, distinct vegetational zonation suggests niche-assembly; however, within vegetational bands, there is considerable small-scale spatial variation suggesting stochastic properties. en
dc.relation.ispartof Palaeogeography palaeoclimatology palaeoecology en
dc.title Vegetational zonation in a swamp forest, Middle Pennsylvanian, Illinois Basin, U.S.A., indicates niche differentiation in a wetland plant community en
dc.type Journal Article en
dc.identifier.srbnumber 143547
dc.identifier.doi 10.1016/j.palaeo.2017.08.020
rft.jtitle Palaeogeography palaeoclimatology palaeoecology
rft.volume 487
rft.spage 71
rft.epage 92
dc.description.SIUnit NH-Paleobiology en
dc.description.SIUnit NMNH en
dc.description.SIUnit Peer-reviewed en
dc.citation.spage 71
dc.citation.epage 92


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search DSpace


Browse

My Account