Skip to main content
Log in

Microbathymetry inferences from two AUV dives over a short segment of the Central Indian Ridge between 10°18′ and 10°57′S, Indian Ocean

  • Research
  • Published:
Geo-Marine Letters Aims and scope Submit manuscript

Abstract

The topographic fabric of the rift valley floor has been analyzed using the multibeam echosounder data obtained by the autonomous underwater vehicle (AUV) Abyss at two locations over a short segment of the slow-spreading Central Indian Ridge between 10°18′ and 10°57′S. The region is influenced by hydrothermal venting in the near vicinity. Two AUV dives D51 and D52 were performed over this segment at two locations that are 30 km apart and covered 5 km2 and 8 km2 seafloor area, respectively. The dive D51 covered the off-axis part of the rift valley floor in the middle part of the segment, and the dive D52 is located near to the non-transform discontinuity that covered the terminal part of an oceanic core complex (OCC). High-resolution seafloor topography as revealed by the AUV-mounted multibeam echosounder system brought out several micro-bathymetric fabric features such as a lava lake, a cratered volcano, an OCC, and the foot wall volcanic complex at the distal part of the OCC. The valley floor imaged in the D51 is marked by a lava flow encompassing an area of 1 km2 and a volcano in the NE corner. The volcano has a diameter of about 800 m with an elevation of about 200 m from the adjacent seafloor, and the partially mapped volcano crater has a relief of about 60 m. A prominent linear fissure running parallel to the ridge axis has been identified; this feature joins with the volcano. Analysis of AUV-mounted CTD data indicated three distinct temperature spikes ranging 0.009 to 0.013 °C in the region of dive D51. The observed temperature spikes appear to be related to the linear fissure on the seafloor and probably represent leaky venting of fluids from the fissure. With respect to the dive D52, the foot wall volcanic features associated with the OCC are prominent. The volcanic seafloor feature covered an area of 3.45 km2 and is conspicuous with rugged topographic fabric at the base of the OCC. These inferences and the morphotectonics of the rift valley floor as revealed by the AUV data suggest moderate hydrothermal venting in this segment of the slow-spreading Central Indian Ridge.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5

Similar content being viewed by others

Data availability

All the data presented in the study are acquired by us and will be made available through http://ramadda.npdc.ncpor.res.in/repository/entry/show?entryid=271d636c-6ea6-4bc3-bdc8-4a6ffe14f050

Code availability

Not applicable.

References

Download references

Acknowledgements

The authors thank Prof. Sunil Kumar Singh, Director, CSIR-NIO, and Dr. M. Ravichandran, Secretary, MoES, and former Director of NCPOR, for encouraging this study. The data was acquired as a part of the Ministry of Earth Sciences, Government of India–funded program. Thanks to the captain and crew members of ORV Sagar Nidhi-48 cruise for their support. The authors are thankful to the ABYSS, GEOMAR team, and Dr. Colin Devey, GEOMAR, for providing the AUV and coordinating the AUV charter process. Mr. Desmond Gracias of CSIR-NIO, Goa is thanked for excellent onboard technical support. All the figures are plotted with the Generic Mapping Tools (Wessel et al., 2019). The authors thank Dr. Gabriele Uenzelmann-Neben, Editor, Geo-Marine Letters, for the encouragement. The authors thank the reviewer Dr. M. Rodriguez and other anonymous reviewers for the encouraging comments, critical review, and suggestions that helped us to improve the MS. This is CSIR-NIO contribution 7006 and NCPOR contribution J-51/2022-23.

Funding

This study was funded by the CSIR-National Institute of Oceanography, India (Grant No. 30-(2050)/COR06/2003-Finance), the Ministry of Earth Sciences, India (Grant No. MoES/Hydro-Sulphides/04/08-PC-II), and the Ministry of Earth Sciences, India (Grant No. MOES/EFC/28/2018-II).

Author information

Authors and Affiliations

Authors

Contributions

KAK coordinated the project and participated in data acquisition, processing, and interpretation. KAK, VY, and AS wrote the paper. AS and LS prepared the figures. VY, AS, and LS participated in data acquisition. DR participated in data acquisition and reviewed the manuscript. NA provided AUV monitoring and support, coordinated with the onboard AUV team, and participated in the acquisition, processing, and interpretation of AUV data. KS and AM participated in the data acquisition. PJK reviewed the manuscript. All authors read and approved the final manuscript.

Corresponding author

Correspondence to K. A. Kamesh Raju.

Ethics declarations

Competing interests

The authors declare no competing interests.

Ethics approval

Not applicable.

Consent to participate

Not applicable.

Consent for publication

Not applicable.

Conflict of interest

The authors declare no competing interests.

Additional information

Publisher's note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Raju, K.A.K., Yatheesh, V., Rao, A.S. et al. Microbathymetry inferences from two AUV dives over a short segment of the Central Indian Ridge between 10°18′ and 10°57′S, Indian Ocean. Geo-Mar Lett 43, 1 (2023). https://doi.org/10.1007/s00367-022-00742-x

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s00367-022-00742-x

Navigation