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TitleThe Bajocian (Middle Jurassic): a key interval in the early Mesozoic phytoplankton radiation
AuthorWiggan, N J; Riding, J B; Fensome, R A; Mattioli, E
SourceEarth-Science Reviews vol. 180, 2018 p. 126-146, https://doi.org/10.1016/j.earscirev.2018.03.009
Year2018
Alt SeriesNatural Resources Canada, Contribution Series 20170383
PublisherElsevier
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf; html
ProvinceCanada; British Columbia; Alberta; Saskatchewan; Manitoba; Ontario; Quebec; New Brunswick; Nova Scotia; Prince Edward Island; Newfoundland and Labrador; Northwest Territories; Yukon; Nunavut
NTS1; 2; 3; 10; 11; 12; 13; 14; 15; 16; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 52; 53; 54; 55; 56; 57; 58; 59; 62; 63; 64; 65; 66; 67; 68; 69; 72; 73; 74; 75; 76; 77; 78; 79; 82; 83; 84; 85; 86; 87; 88; 89; 92; 93; 94; 95; 96; 97; 98; 99; 102; 103; 104; 105; 106; 107; 114O; 114P; 115; 116; 117; 120; 340; 560
Areaworld
Lat/Long WENS-180.0000 180.0000 90.0000 -90.0000
Subjectspaleontology; Middle Jurassic; Bajocian; Bathonian; micropaleontology; microfossils; macrofossils; fossil distribution, geographic; dispersal patterns; evolution; paleoecology; paleogeography; paleoclimatology; paleo-sea levels; paleoenvironment; Phytoplankton; Dinoflagellates; Gonyaulacaceae; Dissiliodinium; Coccolithophores; Watznaueria; Tethys Ocean; Hispanic Corridor; paleoceanography; Phanerozoic; Mesozoic; Jurassic
Illustrationsbiostratigraphic charts; graphs; sketches; lithologic sections; geoscientific sketch maps; bar graphs; photomicrographs; geochronological charts
ProgramWestern Arctic Sverdrup Basin, GEM2: Geo-mapping for Energy and Minerals
AbstractDinoflagellates and coccolithophores are two of the most important groups of phytoplankton in the modern oceans. These groups originated in the Triassic and radiated through the early Mesozoic, rising to ecological prominence. Within this long-term radiation, important short-term intervals of evolutionary and ecological change can be recognised. The Bajocian (Middle Jurassic, ~170-168 Ma) was characterised by an important ecological transition within the coccolithophores, and the radiation of one of the principal families of cyst-forming dinoflagellates, the Gonyaulacaceae. During the Early Bajocian, the coccolith genus Watznaueria diversified and expanded ecologically to dominate coccolith floras, a situation which continued for the remainder of the Mesozoic. This pattern was paralleled within dinoflagellate cyst floras by the ecological dominance of the genus Dissiliodinium in the mid-palaeolatitudes. These phenomena appear to be linked to a positive carbon isotope shift, and an interval of enhanced productivity driven by a shift to a more humid climate, enhanced continental weathering and nutrient flux, or by changes in ocean circulation and upwelling. The latest Early Bajocian to earliest Bathonian was then characterised by the rapid increase in diversity of dinoflagellate cysts within the family Gonyaulacaceae. Through this interval, the Gonyaulacaceae transitioned from being a relatively minor component of dinoflagellate cyst floras, to becoming one of the prominent groups of cyst-forming dinoflagellates, which has persisted to the Holocene. In Europe, the pattern of this radiation was strongly influenced by sea level, with the increase in gonyaulacacean diversity reflecting a major second-order transgression. On a finer scale, the main pulses of first appearances correlate with third-order transgressive episodes. A rise in sea level, coupled with changes in the tectonic configuration of ocean gateways, appears to have controlled the pattern of plankton diversification in Europe. These palaeoceanographic changes may have enhanced water-mass transfer between Europe, the northwest Tethys Ocean and the Hispanic Corridor, which promoted the floral interchange of dinoflagellates. Whilst sea-level rise and associated large-scale palaeoenvironmental shifts appear to have controlled the pattern of dinoflagellate cyst appearances in several regions outside Europe, there is no direct correlation between dinoflagellate cyst diversity and sea-level rise on a global scale. Although the Bajocian was transgressive in several regions, widespread flooded continental area was also present throughout the preceding Aalenian, an interval of low gonyaulacacean diversity. Moreover, although the Middle Jurassic was an interval of major climatic cooling, there was a ~5 myr gap between the onset of cooling and the radiation of gonyaulacaceans during the Bajocian. The Bajocian was, however, marked by a major evolutionary radiation in the pelagic realm, including ammonites, giant suspension feeding fishes and planktonic foraminifera. These phenomena may indicate an underlying ecological driver to the radiation of dinoflagellates during the Bajocian evolutionary explosion which could represent an extension of the Mesozoic Marine Revolution.
Summary(Plain Language Summary, not published)
The greatest extinction occurred 250 million years ago. The taxa that remained became the ancestors of modern organisms, and determined the pattern of evolution for the next 100 million years. The marine food web was largely re-invented, with new groups such as the dinoflagellates and coccolithophores evolving. Both groups left sufficient fossils (as dinoflagellate cysts and coccoliths) to enable investigation of the details of their evolutionary pathways in the Triassic through Middle Jurassic. Major developments in these groups occurred in the Middle Jurassic Bajocian stage, contemporaneous with significant climatic, sea-level, tectonic and ecological changes. In the paper we suggest that changing oceanic seaways and basins may have promoted changes in food change dynamics that are responsible for changes that we see in the dinoflagellate and coccolithophore fossil records in the Bajocian. The Western Arctic contains Bajocian sediments that remain poorly investigated, and thus a potential area of study for comparison of the trends observed in this paper.
GEOSCAN ID308074