| Volumes and Issues Contents of Issue 3 Special Issue |
www.biogeosciences-discuss.net/3/575/2006/
© Author(s) 2006. This work is licensed
under a Creative Commons License.
An importance of diazotrophic cyanobacteria as a primary producer during Cretaceous Oceanic Anoxic Event 2
1Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-cho Yokosuka 237-0061, Japan
2Department of Earth and Planetary Sciences, University of Tokyo, Hongo Bunkyo-ku Tokyo133-0033, Japan
3Ocean Research Institute, University of Tokyo, 1-15-1 Minamidai, Nakano-ku Tokyo 164-8639, Japan
Abstract. In Livello Bonarelli black shale deposited during Cretaceous Oceanic Anoxic Event 2 (OAE-2, ca. 94 Ma), nitrogen isotopic compositions of bulk sediments are in a narrow range from −2.7 to −0.7. We also determined molecular distribution and nitrogen isotopic compositions of geoporphyrins extracted from the black shale. The nitrogen isotopic compositions of C32 Ni deoxophylloerythroetioporphyrin (DPEP) and total Ni porphyrins are −3.5 and −3.3, respectively, leading us to the estimation that the mean nitrogen isotopic composition of photoautotrophic cell was around +1 during the formation of Bonarelli black shale. This value is suggestive of N2-fixation a dominant process for these photoautotrophs when assimilating nitrogen. Furthermore, Ni-chelated C32 DPEP, derived mainly from chlorophyll a was the highest concentration. Based on these evidence, we conclude that diazotrophic cyanobacteria were major primary producers during that time. The cyanobacteria may be key photoautotrophs during the formation of black shale type sediments intermittently observed throughout the later half of the Earth's history, and hence may have played a crucial role in the evolution of geochemical cycles.
Discussion Paper (PDF, 860 KB) Interactive Discussion (Closed, 3 Comments) Final Revised Paper (BG)
Citation: Ohkouchi, N., Kashiyama, Y., Kuroda, J., Ogawa, N. O., and Kitazato, H.: An importance of diazotrophic cyanobacteria as a primary producer during Cretaceous Oceanic Anoxic Event 2, Biogeosciences Discuss., 3, 575-605, 2006. Bibtex EndNote Reference Manager
