Asia

Biostratigraphy and paleoenvironment reconstructions.
High resolution geological and paleogeographical maps.
Organic matter characterization.

Asia

Biostratigraphy and paleoenvironment reconstructions.
High resolution geological and paleogeographical maps.
Organic matter characterization.
CHINA

      Junggar Basin, ©L. Barier

CHINA

Junggar Basin, ©L. Barier

CHINA

Junggar Basin, ©L. Barier

CHINA

Junggar Basin, ©L. Barier

CHINA

Rain forest – Hainan Isle

CHINA

Rain Forest – Hainan Isle

CHINA

Rain forest – Hua Ping

Myanmar
Myanmar
Myanmar
Myanmar
China

Rain Forest with Taxodium distichum – Hua Ping

 

Mongolia

Industrial project: Biostratigraphic correlations and paleoenvironment dynamics based on palynological analysis (Cretaceous), Zuunbayan & Uneget Basins.

 

China

Academic  project: Insight into Tian Shan topography prior to the onset of the Himalayan orogenic cycle: tectonics and climate inferences.

Academic project : Cathaya: past and present-day distribution and paleoecology.

Cathaya is the Chinese emblematic tree, represented today by only one species, Cathaya argyrophylla Chun & Kuang, restricted in a ten of scattered altitudinal localities (900-1,700 m) in the subtropical China. During the whole Tertiary, the genus was largely distributed in Eurasia and North America with probably several species.

 

Myanmar

Industrial project: High-resolution multi-proxy biostratigraphy (Paleocene – Quaternary) paleoenvironmental and paleogeographic reconstructions, Myanmar. 

Multi-proxy analyses (analyses of calcareous nannoplankton, foraminifera, pollen grains, dinoflagellate cysts, palynofacies and organic geochemistry were performed on samples from a Myanmar onshorre block, in order to provide high-resolution biostratigraphy, geological and paleogeographical detailed maps, and organic matter characterization. The studied samples cover the following sedimentological regional formations: Kanbala, Taunggale, Pondaung and Yaw covering the Eocene; Shezetaw, Padaung, and Okhmitaung corresponding to the Oligocene; Pyawbwe, Kyaukkok and Obogon representative of late – middle Miocene; and the Irrawaddy Group (middle Miocene-late Quaternary).

The proposed ages by the regional stratigraphy have been seriously questioned for 30% of the samples. Six paleogeographical maps, running from the Paleocene to mid-Miocene are proposed, based on biostratigraphical and paleoenvironmental results.

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