A Late Ordovician age for the Whirlpool and Power Glen formations, New York

2016 ◽  
Vol 53 (7) ◽  
pp. 739-747 ◽  
Author(s):  
Laurenz Schröer ◽  
Thijs R.A. Vandenbroucke ◽  
Olle Hints ◽  
Thomas Steeman ◽  
Jacques Verniers ◽  
...  

A restudy of the palynology of the Whirlpool Formation and Power Glen Formation in New York (USA) yielded a diverse fossil assemblage with cryptospores, glomalean fungi, acritarchs, chitinozoans, scolecodonts, and small carbonaceous fossils. These new data, and particularly the presence of the chitinozoan index fossil Hercochitina crickmayi, combined with emerging stable carbon isotope data, suggest a Late Ordovician (Katian or Hirnantian) age for these formations, which is older than their previously suggested Silurian (Rhuddanian) age.

2016 ◽  
Vol 129 ◽  
pp. 249-258 ◽  
Author(s):  
Brad E. Rosenheim ◽  
Matthew A. Pendergraft ◽  
George C. Flowers ◽  
Robert Carney ◽  
José L. Sericano ◽  
...  

Oecologia ◽  
2001 ◽  
Vol 129 (1) ◽  
pp. 106-113 ◽  
Author(s):  
Marie-Anne Delègue ◽  
Marc Fuhr ◽  
Dominique Schwartz ◽  
André Mariotti ◽  
Robert Nasi

2020 ◽  
Vol 26 (12) ◽  
pp. 7158-7172
Author(s):  
Aliénor Lavergne ◽  
David Sandoval ◽  
Vincent J. Hare ◽  
Heather Graven ◽  
Iain Colin Prentice

2021 ◽  
Vol 18 (20) ◽  
pp. 5719-5728
Author(s):  
Zofia Dubicka ◽  
Maria Gajewska ◽  
Wojciech Kozłowski ◽  
Pamela Hallock ◽  
Johann Hohenegger

Abstract. Photosynthetically active foraminifera are prolific carbonate producers in warm, sunlit, surface waters of the oceans. Foraminifera have repeatedly developed mixotrophic strategies (i.e., the ability of an organism or holobiont to both feed and photosynthesize) by facultative or obligate endosymbiosis with microalgae or by sequestering plastids (kleptoplasts) of ingested algae. Mixotrophy provides access to essential nutrients (e.g., N, P) through feeding while providing carbohydrates and lipids produced through photosynthesis, resulting in substantial energetic advantage in warm, sunlit environments where food and dissolved nutrients are scarce. Our morphological as well as stable carbon isotope data provide, as of now, the earliest (Mid-Devonian) evidence for photosynthetic activity in the first advanced, multichambered, calcareous foraminifera, Semitextularia, from the tropical shelf of the Laurussia paleocontinent. This adaptation likely influenced the evolutionary radiation of calcareous Foraminifera in the Devonian (“Givetian revolution”), one of the most important evolutionary events in foraminiferal history, that coincided with the worldwide development of diverse calcifying marine communities inhabiting shelf environments linked with Devonian stromatoporoid coral reefs.


2017 ◽  
Vol 63 (2) ◽  
pp. 570-587 ◽  
Author(s):  
Jeff R. Havig ◽  
Trinity L. Hamilton ◽  
Michael McCormick ◽  
Brianna McClure ◽  
Todd Sowers ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document