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Mahyar Mohtadi

Biographic Data

ID4783517
NAMEMahyar Mohtadi
GIVEN NAMESMahyar
FAMILY NAMEMohtadi
SIGNATUREMOHTADI M
AFFILIATIONSUniversity of Bremen
ORCID0000-0003-3306-0969
VERIFIEDYes
TOTAL WORKS3
TOTAL CITATIONS2
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2006
LATEST PUBLICATION YEAR2019
H-INDEX1
  • Dissolved inorganic Radiocarbon content of the Western Coral sea

    Open Access•Aymeric PM Servettaz, Yūsuke Yokoyama et al.•ARTICLE•Radiocarbon•2019•References: 46

    The South Pacific Ocean contributes to the global carbon cycle by exchanging CO 2 between the atmosphere and intermediate to deep water masses. The path of the Antarctic Intermediate Water (AAIW) in the South Pacific gyre has been inferred from salinity, oxygen, and nutrient measurements, but radiocarbon ( 14 C) measurements—a direct tracer of the carbon cycle—remain sparse. Here, we present the first radiocarbon profiles in the western Coral Sea…

  • Planktonic Foram Dates from the Indonesian Arc

    Open Access•John Southon, Mahyar Mohtadi et al.•ARTICLE•Radiocarbon•2013•Cited by: 2•References: 18

    The Indonesian Arc represents the subduction of the Indian-Australian plate beneath Asia. It has been the scene of catastrophic tectonic activity, including the recent 2004 M=9.1 Aceh earthquake and resulting Indian Ocean tsunami. We have dated planktonic forams associated with historic tephras (Tambora, 1815 and Krakatau, 1883) in marine sediment cores to determine radiocarbon reservoir ages for 2 locations along the arc. Our best estimates for …

  • The late quaternary paleoenvironment of Chile as seen from marine archives

    Open Access•Jan-Berend W Stuut, Margarita Marchant et al.•ARTICLE•Geographica Helvetica•2006

    Many variables have been used to reconstruct Chilean paleoenvironmental changes during the late Quaternary. In this paper we present an overview of a number of these variables, so-called proxies, that have been inferred from marine sediments from the Chilean continental margin and summarise the results. In general, a glacial-interglacial pattern of climate changes can be recognised in the proxy records with high-frequency variabilities superposed…

  • Planktonic Foram Dates from the Indonesian Arc

    Open Access•John Southon, Mahyar Mohtadi et al.•ARTICLE•Radiocarbon•2013•Cited by: 2•References: 18

    The Indonesian Arc represents the subduction of the Indian-Australian plate beneath Asia. It has been the scene of catastrophic tectonic activity, including the recent 2004 M=9.1 Aceh earthquake and resulting Indian Ocean tsunami. We have dated planktonic forams associated with historic tephras (Tambora, 1815 and Krakatau, 1883) in marine sediment cores to determine radiocarbon reservoir ages for 2 locations along the arc. Our best estimates for …

  • The late quaternary paleoenvironment of Chile as seen from marine archives

    Open Access•Jan-Berend W Stuut, Margarita Marchant et al.•ARTICLE•Geographica Helvetica•2006

    Many variables have been used to reconstruct Chilean paleoenvironmental changes during the late Quaternary. In this paper we present an overview of a number of these variables, so-called proxies, that have been inferred from marine sediments from the Chilean continental margin and summarise the results. In general, a glacial-interglacial pattern of climate changes can be recognised in the proxy records with high-frequency variabilities superposed…

  • Planktonic Foram Dates from the Indonesian Arc

    Open Access•John Southon, Mahyar Mohtadi et al.•ARTICLE•Radiocarbon•2013•Cited by: 2•References: 18

    The Indonesian Arc represents the subduction of the Indian-Australian plate beneath Asia. It has been the scene of catastrophic tectonic activity, including the recent 2004 M=9.1 Aceh earthquake and resulting Indian Ocean tsunami. We have dated planktonic forams associated with historic tephras (Tambora, 1815 and Krakatau, 1883) in marine sediment cores to determine radiocarbon reservoir ages for 2 locations along the arc. Our best estimates for …

  • Dissolved inorganic Radiocarbon content of the Western Coral sea

    Open Access•Aymeric PM Servettaz, Yūsuke Yokoyama et al.•ARTICLE•Radiocarbon•2019•References: 46

    The South Pacific Ocean contributes to the global carbon cycle by exchanging CO 2 between the atmosphere and intermediate to deep water masses. The path of the Antarctic Intermediate Water (AAIW) in the South Pacific gyre has been inferred from salinity, oxygen, and nutrient measurements, but radiocarbon ( 14 C) measurements—a direct tracer of the carbon cycle—remain sparse. Here, we present the first radiocarbon profiles in the western Coral Sea…

Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Oceanography (3 works) · Paleontology (3 works) · Radiocarbon dating (2 works) · Antarctic Intermediate Water (1 work) · Circumpolar deep water (1 work) · Climatology (1 work) · Continental Margin (1 work) · Coral (1 work)

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