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Mississippian
(redirected from Mississippian Period)

   Also found in: Encyclopedia, Wikipedia 0.01 sec.
Mis·sis·sip·pi·an  (ms-sp-n)
adj.
1. Of or relating to the state or residents of Mississippi or the Mississippi River.
2. Of or belonging to the geologic time, system of rocks, or sedimentary deposits of the fifth period of the Paleozoic Era, characterized by the submergence of extensive land areas under shallow seas. See Table at geologic time.
n.
1. A native or resident of Mississippi.
2. The Mississippian Period. Also called Lower Carboniferous.

Mississippian [ˌmɪsɪˈsɪpɪən]
adj
1. (Placename) of or relating to the state of Mississippi or the Mississippi River
2. (Earth Sciences / Geological Science) (in North America) of, denoting, or formed in the lower of two subdivisions of the Carboniferous period (see also Pennsylvanian (sense 2)), which lasted for 30 million years
n
1. (Placename) an inhabitant or native of the state of Mississippi
2. (Earth Sciences / Geological Science) the. the Mississippian period or rock system equivalent to the lower Carboniferous of Europe

Mississippian  (ms-sp-n)
The fifth period of the Paleozoic Era, from about 360 to 320 million years ago. During this time shallow seas spread over former land areas and the first primitive conifers appeared. See Chart at geologic time.
ThesaurusLegend:  Synonyms Related Words Antonyms
Noun1.Mississippian - from 345 million to 310 million years agoMississippian - from 345 million to 310 million years ago; increase of land areas; primitive ammonites; winged insects
Carboniferous, Carboniferous period - from 345 million to 280 million years ago
2.Mississippian - a native or resident of MississippiMississippian - a native or resident of Mississippi
American - a native or inhabitant of the United States


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In the field, this burial appeared to be typical for the transitional Woodland/early Mississippian period.
The exhibition then surveys the Mississippian period (beginning in 800).
Understanding the paleoclimate of the Rheic Ocean at the beginning of the Mississippian Period, throughout the Kinderhookian, will help determine the spatial and temporal limits of the dendroid Graptolite Dictyonema within Missouri.
 
 
 
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