Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2533-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-2533-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Pliocene expansion of C4 vegetation in the Core Monsoon Zone on the Indian Peninsula
Marine Chemistry & Geochemistry, Woods Hole Oceanographic
Institution, Woods Hole, MA 02543, USA
Liviu Giosan
Geology & Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
Yongsong Huang
Department of Earth, Environmental, and Planetary Sciences, Brown
University, Providence, RI 02912, USA
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15 citations as recorded by crossref.
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- Remote and local drivers of Pleistocene South Asian summer monsoon precipitation: A test for future predictions S. Clemens et al. 10.1126/sciadv.abg3848
- Multi-phase ecological change on Indian subcontinent from the late Miocene to Pleistocene recorded in the Nicobar Fan B. House et al. 10.1017/S0016756823000481
- Influences of summer monsoon variations on the terrigenous influx, bioproductivity and early diagenetic changes in the southwest Bay of Bengal during Late Quaternary A. Prajith et al. 10.1016/j.margeo.2022.106825
- Role of land-ocean interactions in stepwise Northern Hemisphere Glaciation Y. Zhong et al. 10.1038/s41467-024-51127-w
- Silicate weathering linked with global climate change along the Mid-Pleistocene transition: A record from the Himalayan foreland Basin, India M. Chauhan et al. 10.1016/j.catena.2024.108047
- Carbon isotopic ratios of modern C3 and C4 vegetation on the Indian peninsula and changes along the plant–soil–river continuum – implications for vegetation reconstructions F. Kirkels et al. 10.5194/bg-19-4107-2022
- A synthesis of monsoon exploration in the Asian marginal seas P. Clift et al. 10.5194/sd-31-1-2022
- The late Neogene distribution of C 3 –C 4 plants in the Himalayan Foreland Basin: insight from the δ 13 C values and sedimentological architecture of the Siwaliks S. Ghosh et al. 10.1144/SP549-2023-145
- A Pliocene Precipitation Isotope Proxy‐Model Comparison Assessing the Hydrological Fingerprints of Sea Surface Temperature Gradients S. Knapp et al. 10.1029/2021PA004401
- Revisiting the diachronous transition of C3 to C4 plants in the Himalayan foreland and other parts of the globe: A sedimentological perspective S. Ghosh et al. 10.1111/sed.12865
- When Eastern India Oscillated Between Desert Versus Savannah‐Dominated Vegetation C. Zorzi et al. 10.1029/2022GL099417
- Paleoclimatic and vegetational change in the Siwalik sub-Group of Pakistan and its contemporary geographic regions: a stable isotope perspective M. Waseem et al. 10.1080/08120099.2021.1893221
- Isolating Detrital and Diagenetic Signals in Magnetic Susceptibility Records From Methane‐Bearing Marine Sediments J. Johnson et al. 10.1029/2021GC009867
- Greenhouse Gas and Ice Volume Drive Pleistocene Indian Summer Monsoon Precipitation Isotope Variability S. McGrath et al. 10.1029/2020GL092249
15 citations as recorded by crossref.
- Unlocking the genetic enigma: A paradigm shift towards evidence-based conservation of Indian star tortoise (Geochelone elegans) S. Sahoo et al. 10.1016/j.biocon.2023.110421
- Remote and local drivers of Pleistocene South Asian summer monsoon precipitation: A test for future predictions S. Clemens et al. 10.1126/sciadv.abg3848
- Multi-phase ecological change on Indian subcontinent from the late Miocene to Pleistocene recorded in the Nicobar Fan B. House et al. 10.1017/S0016756823000481
- Influences of summer monsoon variations on the terrigenous influx, bioproductivity and early diagenetic changes in the southwest Bay of Bengal during Late Quaternary A. Prajith et al. 10.1016/j.margeo.2022.106825
- Role of land-ocean interactions in stepwise Northern Hemisphere Glaciation Y. Zhong et al. 10.1038/s41467-024-51127-w
- Silicate weathering linked with global climate change along the Mid-Pleistocene transition: A record from the Himalayan foreland Basin, India M. Chauhan et al. 10.1016/j.catena.2024.108047
- Carbon isotopic ratios of modern C3 and C4 vegetation on the Indian peninsula and changes along the plant–soil–river continuum – implications for vegetation reconstructions F. Kirkels et al. 10.5194/bg-19-4107-2022
- A synthesis of monsoon exploration in the Asian marginal seas P. Clift et al. 10.5194/sd-31-1-2022
- The late Neogene distribution of C 3 –C 4 plants in the Himalayan Foreland Basin: insight from the δ 13 C values and sedimentological architecture of the Siwaliks S. Ghosh et al. 10.1144/SP549-2023-145
- A Pliocene Precipitation Isotope Proxy‐Model Comparison Assessing the Hydrological Fingerprints of Sea Surface Temperature Gradients S. Knapp et al. 10.1029/2021PA004401
- Revisiting the diachronous transition of C3 to C4 plants in the Himalayan foreland and other parts of the globe: A sedimentological perspective S. Ghosh et al. 10.1111/sed.12865
- When Eastern India Oscillated Between Desert Versus Savannah‐Dominated Vegetation C. Zorzi et al. 10.1029/2022GL099417
- Paleoclimatic and vegetational change in the Siwalik sub-Group of Pakistan and its contemporary geographic regions: a stable isotope perspective M. Waseem et al. 10.1080/08120099.2021.1893221
- Isolating Detrital and Diagenetic Signals in Magnetic Susceptibility Records From Methane‐Bearing Marine Sediments J. Johnson et al. 10.1029/2021GC009867
- Greenhouse Gas and Ice Volume Drive Pleistocene Indian Summer Monsoon Precipitation Isotope Variability S. McGrath et al. 10.1029/2020GL092249
Latest update: 20 Nov 2024
Short summary
Over the past 20 Myr, there has been a dramatic global increase in plants using C4 photosynthetic pathways. We analyze C and H isotopes in fatty acids of leaf waxes preserved in marine sediment from the Bay of Bengal to examine changes in photosynthesis in the Core Monsoon Zone of the Indian Peninsula over the past 6 Myr. The observed increase in C4 vegetation from 3.5 to 1.5 Ma is synchronous with C4 expansions in northwest Australia and East Africa, suggesting regional hydroclimate controls
Over the past 20 Myr, there has been a dramatic global increase in plants using C4...