Species Accounts | Fish Primer | Relationships | Morphology
Overview | Invertebrates | Plants | Enigmas
Introduction | Geology | Climate | Deposition | Summary
Suggested Readings | Bibliography | Web Links
Credits | Richard Lund | Eileen Grogan | Fossils Policy | Terms of Use

Climatology

North America in Late Missippian
North American emergent land (brown) and extent of seas (green) during the upper Mississippian. BGL, position of Bear Gulch Limestone; CMT, Central Montana Trough; EQ, equator; 10- 10 degree North latitude; WB, Williston Basin.

Global and Regional Paleogeography

Geomagnetic data place central Montana at about 10-12° north of the equator in Upper Mississippian time, or approximately at the present latitude of the southern Red Sea to the Sudan. The Visean-Namurian North American continent is reconstructed as rotated approximately 45° clockwise relative to its present orientation, with the continental plate moving north. In comparison to today's environments, and all other factors being analogous, Africa's Sahel would best approximate the climatic conditions of the Bear Gulch region; desert conditions are likely to have prevailed further north and more tropical conditions to the south. Because these latitudes are characterized by a monsoonal climatic regime of rainy and dry seasons, the Bear Gulch region is believed to have been subject to similar seasonal conditions resulting from shifts in the Intertropical Convergence Zone (ITCZ), the intensity of which would be defined by the magnitude of the ITCZ shift.

Paleoclimatology

seasonsWhen the ITCZ was positioned closest to the paleo-equator the 10-12° latitude would have been most likely to experience cool, dry east to northeasterly winds during the winter season. Progression from the winter season into spring and summer would have been defined by a northward shift in the ITCZ. As the ITCZ increasingly encroached upon the latitude of the Bear Gulch it would have introduced the increased probability of strong westerly to southwesterly winds and precipitation, and a monsoonal-type summer climate. Refreshment of the bay with epicontinental sea water would have been extremely restricted in summer compared to winter because wind-driven waters could only enter from a southeast channel rather than the bay mouth proper and wind direction would counter the impact of daily tidal flow.

Gypsum typically indicates arid conditions. Gypsum deposits in adjacent Heath Shale facies and gypsum and chert nodules in shallow facies corroborate the semi-arid to arid tropical aspect of the regional paleoclimate. Gypsum in the shallow facies and along the paleo-eastern margin represents periods of high evaporation rate during the hot and dry times as well as the terminal stages of filling in of the bay. There is an almost total absence of fresh-water macrofossils in the Bear Gulch Limestone. This is in spite of the narrowness of the Central Montana Trough and the proximity of the shores of the Bear Gulch bay; conditions that would have provided the shallow, marginal environments ideal to supporting freshwater communities if freshwater were regularly available. The alternative conditions of brackish and fresh water indicator fossils in the Heath paper shale, and the high percentage of the presumed brackish water indicator fish Acanthodes toward the western edge of the Bear Gulch lens, serve as seasonal and climatic counterpoints.

turbiditiesMicroturbidites are the dominant mode of sediment deposition in the Bear Gulch Limestone. Either hypersalinity or fresher-more saline layering could have provided an adequately dense bottom layer for the suspension of a turbidity current composed of very fine particles and particle-organic aggregates. Hypersalinity has previously been used as a mechanism to explain the environment of deposition of the Heath Formation shales to the east. Both conditions fit our seasonal model for the Bear Gulch. Periods of aridity would result in warm, saline waters in the shallows and a denser hypersaline layer of bottom water extending from the bay head region to the zone of epicontinental sea infiltration. A storm or other disturbance of the sediment during a period of density stratification would result in a turbidity flow or detached turbidity current along the pycnocline from the shallow paleo-western margins eastward. Thus the available data support our proposal for seasons of aridity and limited but torrential rainfall in a monsoonal climatic regime. The possible effects of a stratified water column carrying an organic-rich turbidity current into the central basin over a hypersaline lower water layer are discussed below.

Top of page

References

Previous: Geology Next: Deposition

Top of page