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Journals / Maden Tetkik ve Arama Dergisi / 1999 / Cilt: 121 - Sayı: 121

PALEONTOLOGICAL (PLANKTIC FORAMINIFER-OSTRACOD) INVESTIGATION OF EOCENE SEQUENCE OF KARAMAN REGION

Ümit ŞAFAK
Pages
1–1
Publication Date
1999-02-01
DOI
—
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

In addition, ostracod species described were stratigraphically and paleogeographically compared with those of other basins.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:The microfauna of Eocene sequence outcropping around Karaman have been investigated.
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Key Findings & Data:These planktic foraminifers and ostracods were systematically described; also Acarinina bullbrooki planktic foraminifer zone belonging to Lutetian has been determined and this zone was compared with other Eocene planktic foraminifer zones over the world indicating same level.
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Conclusion & Impact:In addition, ostracod species described were stratigraphically and paleogeographically compared with those of other basins.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Domain Parameters

Abstract

The microfauna of Eocene sequence outcropping around Karaman have been investigated. These planktic foraminifers and ostracods were systematically described; also Acarinina bullbrooki planktic foraminifer zone belonging to Lutetian has been determined and this zone was compared with other Eocene planktic foraminifer zones over the world indicating same level. In addition, ostracod species described were stratigraphically and paleogeographically compared with those of other basins.

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Cite This Article

ŞAFAK, Ü. (1999). PALEONTOLOGICAL (PLANKTIC FORAMINIFER-OSTRACOD) INVESTIGATION OF EOCENE SEQUENCE OF KARAMAN REGION. Maden Tetkik ve Arama Dergisi, Cilt: 121 - Sayı: 121, 1–1. https://ajindex.com/articles/54209

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