Maud J.M. Meijers , Tamás Mikes , Bora Rojay , Erkan Aydar , H. Evren Çubukçu , Thomas Wagner , Tina Lüdecke , Emilija Krsnik , Jens Fiebig , Andreas Mulch
{"title":"中新世安纳托利亚高原内部(t<s:1> rkiye)与现代山地边缘的表面隆起解耦","authors":"Maud J.M. Meijers , Tamás Mikes , Bora Rojay , Erkan Aydar , H. Evren Çubukçu , Thomas Wagner , Tina Lüdecke , Emilija Krsnik , Jens Fiebig , Andreas Mulch","doi":"10.1016/j.epsl.2025.119414","DOIUrl":null,"url":null,"abstract":"<div><div>The Central Anatolian Plateau (CAP) forms the western portion of the Turkish-Iranian plateau and has mostly remained above sea level since ca. 41 Ma. However, the current topography of the CAP has predominantly developed since the Late Miocene, with mean elevations of ca. 1.0–1.5 km and northern and southern mountainous margins with peak elevations that locally exceed 3 km. To clarify patterns of surface uplift, we present paleoelevation estimates for the past 10 Ma by applying stable isotope paleoaltimetry on soil carbonates from the CAP and nearby coastal regions, as well as dual clumped isotope paleothermometry.</div><div>The compiled datasets from the Aegean-Anatolian region display a sustained increase in δ<sup>18</sup>O values of soil carbonates after the Miocene, in response to increased regional aridification. Our paleoaltimetry and dual clumped isotope results indicate that the CAP has been at higher elevations than the modern coastal regions since 10 Ma. By ca. 8 − 6 Ma, our refined paleoaltimetry estimates indicate the presence of a ca. 1.5 km-high orographic barrier. However, surface uplift of the Tauride and Pontide mountains on the southern and northern plateau margin postdate surface uplift of the CAP. Therefore, surface uplift of the CAP and its mountainous margins were decoupled during the Late Miocene, implying distinct geodynamic drivers for their asynchronous formation. Given that the Tauride Mts. emerged from the Mediterranean after 7 Ma, we document outward growth of the southern plateau margin since the Late Miocene.</div></div>","PeriodicalId":11481,"journal":{"name":"Earth and Planetary Science Letters","volume":"663 ","pages":"Article 119414"},"PeriodicalIF":4.8000,"publicationDate":"2025-05-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Miocene decoupling of surface uplift of the Central Anatolian Plateau interior (Türkiye) and its modern mountainous margins\",\"authors\":\"Maud J.M. Meijers , Tamás Mikes , Bora Rojay , Erkan Aydar , H. Evren Çubukçu , Thomas Wagner , Tina Lüdecke , Emilija Krsnik , Jens Fiebig , Andreas Mulch\",\"doi\":\"10.1016/j.epsl.2025.119414\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The Central Anatolian Plateau (CAP) forms the western portion of the Turkish-Iranian plateau and has mostly remained above sea level since ca. 41 Ma. However, the current topography of the CAP has predominantly developed since the Late Miocene, with mean elevations of ca. 1.0–1.5 km and northern and southern mountainous margins with peak elevations that locally exceed 3 km. To clarify patterns of surface uplift, we present paleoelevation estimates for the past 10 Ma by applying stable isotope paleoaltimetry on soil carbonates from the CAP and nearby coastal regions, as well as dual clumped isotope paleothermometry.</div><div>The compiled datasets from the Aegean-Anatolian region display a sustained increase in δ<sup>18</sup>O values of soil carbonates after the Miocene, in response to increased regional aridification. Our paleoaltimetry and dual clumped isotope results indicate that the CAP has been at higher elevations than the modern coastal regions since 10 Ma. By ca. 8 − 6 Ma, our refined paleoaltimetry estimates indicate the presence of a ca. 1.5 km-high orographic barrier. However, surface uplift of the Tauride and Pontide mountains on the southern and northern plateau margin postdate surface uplift of the CAP. Therefore, surface uplift of the CAP and its mountainous margins were decoupled during the Late Miocene, implying distinct geodynamic drivers for their asynchronous formation. Given that the Tauride Mts. emerged from the Mediterranean after 7 Ma, we document outward growth of the southern plateau margin since the Late Miocene.</div></div>\",\"PeriodicalId\":11481,\"journal\":{\"name\":\"Earth and Planetary Science Letters\",\"volume\":\"663 \",\"pages\":\"Article 119414\"},\"PeriodicalIF\":4.8000,\"publicationDate\":\"2025-05-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Earth and Planetary Science Letters\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0012821X25002134\",\"RegionNum\":1,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth and Planetary Science Letters","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0012821X25002134","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Miocene decoupling of surface uplift of the Central Anatolian Plateau interior (Türkiye) and its modern mountainous margins
The Central Anatolian Plateau (CAP) forms the western portion of the Turkish-Iranian plateau and has mostly remained above sea level since ca. 41 Ma. However, the current topography of the CAP has predominantly developed since the Late Miocene, with mean elevations of ca. 1.0–1.5 km and northern and southern mountainous margins with peak elevations that locally exceed 3 km. To clarify patterns of surface uplift, we present paleoelevation estimates for the past 10 Ma by applying stable isotope paleoaltimetry on soil carbonates from the CAP and nearby coastal regions, as well as dual clumped isotope paleothermometry.
The compiled datasets from the Aegean-Anatolian region display a sustained increase in δ18O values of soil carbonates after the Miocene, in response to increased regional aridification. Our paleoaltimetry and dual clumped isotope results indicate that the CAP has been at higher elevations than the modern coastal regions since 10 Ma. By ca. 8 − 6 Ma, our refined paleoaltimetry estimates indicate the presence of a ca. 1.5 km-high orographic barrier. However, surface uplift of the Tauride and Pontide mountains on the southern and northern plateau margin postdate surface uplift of the CAP. Therefore, surface uplift of the CAP and its mountainous margins were decoupled during the Late Miocene, implying distinct geodynamic drivers for their asynchronous formation. Given that the Tauride Mts. emerged from the Mediterranean after 7 Ma, we document outward growth of the southern plateau margin since the Late Miocene.
期刊介绍:
Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.