The Mid-Pleistocene to Holocene Evolution of the Maldives Carbonate Platform Paul, A
Total Page:16
File Type:pdf, Size:1020Kb
VU Research Portal The Mid-Pleistocene to Holocene evolution of the Maldives carbonate platform Paul, A. 2014 document version Publisher's PDF, also known as Version of record Link to publication in VU Research Portal citation for published version (APA) Paul, A. (2014). The Mid-Pleistocene to Holocene evolution of the Maldives carbonate platform. General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal ? Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. E-mail address: [email protected] Download date: 06. Oct. 2021 The Mid-Pleistocene to Holocene evolution of the Maldives carbonate platform Andreas Paul The research reported in this thesis was carried out at the VU University (Vrije Universiteit) Amsterdam in close collaboration with the University of Hamburg. ISBN: 978-94-6259-109-7 © 2014, Andreas Paul Contact: andreas.paul.phd (at) gmail.com Document prepared with LATEX 2ε and typeset by pdfTEX Printed by: Ipskamp Drukkers On the cover: Panoramic view from the upper deck of the German research vessel Meteor while entering the Malé atoll in order to record seismic data. A faint submerged atoll can be seen in the background. VRIJE UNIVERSITEIT The Mid-Pleistocene to Holocene evolution of the Maldives carbonate platform ACADEMISCH PROEFSCHRIFT ter verkrijging van de graad Doctor aan de Vrije Universiteit Amsterdam, op gezag van de rector magnificus prof.dr. F.A. van der Duyn Schouten, in het openbaar te verdedigen ten overstaan van de promotiecommissie van de Faculteit der Aard- en Levenswetenschappen op vrijdag 9 mei 2014 om 13.45 uur in de aula van de universiteit, De Boelelaan 1105 door Andreas Paul geboren te Altenburg, Duitsland promotoren: prof.dr. J.J.G. Reijmer prof.dr. C. Betzler beoordelingscommissie: prof.dr. D. Kroon prof.dr. P.K. Swart dr. A. Brasier dr. F. Mienis dr. L. Reuning voor Pauli & meinen Eltern “We feel surprise when travelers tell us of the vast dimensions of the Pyramids and other great ruins, but how utterly insignificant are the greatest of these, when compared to these mountains of stone accumulated by the agency of various minute and tender animals!“ “We voelen ons overweldigd, als reizigers ons vertellen over de kolossale afmetingen van de piramiden en andere beduidende ruïnen. Maar hoe betekenisloos zijn deze ruïnes als zij worden vergeleken met deze stenen gebergten welke geaccumuleerd zijn door het werk van talrijke minuscule en fragiele diertjes!“ “Wir fühlen uns überwähltigt, wenn Reisende uns von den kolossalen Ausmaßen der Pyramiden und anderer bedeutender Ruinen erzählen. Aber wie vollkommen bedeutungslos sind diese Ruinen verglichen mit jenen steinernen Gebirgen, angehäuft durch die Arbeit von unzähligen winzigen und zerbrechlichen Tierchen!“ Charles Darwin, 1839 Contents Acknowledgements VII English Summaries XI Nederlandse Samenvattingen XVII Deutsche Zusammenfassungen XXIII Introduction 2 A brief overview of the Maldives ................... 2 Charles Darwin and his ideas on atoll formation .......... 4 The Maldives and the Indian Monsoon ............... 9 The geologic setting and development of the Maldives ...... 11 Aims and Objectives .......................... 15 1 The relationship between Late Pleistocene sea-level vari- ations, carbonate platform morphology and shallow- water carbonate production 22 1.1 Introduction ............................. 23 1.1.1 Highstand shedding ..................... 23 1.1.2 Sea-level history ....................... 23 1.1.3 Aims and Objectives .................... 25 1.2 Material and Methods ....................... 26 1.2.1 Planktonic stable oxygen isotopes ............ 26 1.2.2 Nannofossil biostratigraphy ................ 27 I Contents 1.2.3 Radiocarbon dating ..................... 27 1.2.4 X-ray diffraction ....................... 27 1.2.5 Grain-size analysis ...................... 28 1.2.6 Calcium carbonate content and organic carbon .... 28 1.2.7 Mass accumulation rates .................. 29 1.3 Results ................................ 30 1.3.1 Core description ....................... 30 1.3.2 Planktonic oxygen isotopes ................ 30 1.3.3 Nannofossil biostratigraphy and radiocarbon dating .. 30 1.3.4 Age model .......................... 31 1.3.5 Carbonate mineralogy ................... 33 1.3.6 Grain size distributions ................... 35 1.3.7 Calcium carbonate content and organic carbon .... 35 1.3.8 Mass accumulation rates .................. 36 1.4 Discussion .............................. 36 1.4.1 Origin of sedimentary components ............ 36 1.4.2 Flooding and exposure during the past 150,000 years . 40 1.4.3 Comparison with other carbonate platforms ...... 47 1.5 Conclusions ............................. 49 2 Rapid characterisation of carbonate peri-platform ooze using XRF scanning and multivariate statistics 54 2.1 Introduction ............................. 55 2.1.1 Pleistocene shallow-water carbonate facies ....... 55 2.1.2 Multivariate statistical analysis .............. 58 2.1.3 Aims and Objectives .................... 59 2.2 Material and Methods ....................... 59 2.2.1 X-ray fluorescence scanning ................ 60 2.3 Results ................................ 62 2.3.1 Core description ....................... 62 II Contents 2.3.2 Stratigraphy and Age model ................ 62 2.3.3 Proxy records ......................... 63 2.3.4 X-ray fluorescence scanning ................ 63 2.3.5 Element-to-Aragonite transfer function ......... 65 2.4 Multivariate statistical analyses ................. 68 2.4.1 Principal component analysis on full dataset (PCA 1) 70 2.4.2 Principal component analysis selected elements (PCA 2) 71 2.4.3 Sample scores......................... 73 2.5 Discussion.............................. 78 2.5.1 Significance of individual elemental counts in Maldivian peri-platform ooze ...................... 78 2.5.2 Characterisation of the Maldives depositional environ- ment using X-ray fluorescence and multivariate statistics 82 2.6 Conclusions............................. 85 3 The impact of current amplification on sedimentation processes at slopes of the Inner Sea 88 3.1 Introduction............................. 89 3.2 Material and Methods....................... 90 3.2.1 Parasound echo sounding................. 90 3.2.2 Sediment cores and analyses................ 91 3.3 Results................................ 91 3.3.1 Parasound echo sounding................. 91 3.3.2 Sedimentary record of the Ari core (M74/4-1150)... 93 3.3.3 Core-to-seismic tie and stratigraphy ........... 99 3.4 Discussion .............................. 103 3.4.1 Late Pleistocene sequence stratigraphy ......... 103 3.4.2 Glacial-Interglacial variability on the Maldives carbonate platform ............................ 106 3.5 Conclusions ............................. 110 III Contents 4 Late Pleistocene sedimentation patterns within the Inner Sea 114 4.1 Introduction............................. 115 4.2 Material and Methods....................... 116 4.3 Results................................ 118 4.3.1 Core description....................... 118 4.3.2 Biostratigraphy....................... 118 4.3.3 Age model and sedimentation rates ........... 120 4.3.4 Proxy records ......................... 121 4.3.5 Comparison with toe-of-slope cores ............ 122 4.4 Discussion .............................. 124 4.4.1 Sedimentation patterns within the Inner Sea of the Mal- dives carbonate platform .................. 124 4.5 Conclusions ............................. 129 Concluding Remarks 134 Morphology ................................ 134 Sediments ................................. 134 The Maldives vs. Great Bahama Bank ............... 135 A glimpse into the future ........................ 135 References 140 List of Figures 160 List of Tables 164 About the Author 166 IV Acknowledgements This thesis is the result of the cooperation between the department of Sedimentology and Marine Geology at the VU University Amsterdam and the Geological and Palaeontological Institute at the University of Hamburg, under supervision of Prof.Dr. John Reijmer (Amsterdam) and Prof.Dr. Christian Betzler (Hamburg), and a lot more people involved over the course of the years. John, heel erg bedankt voor alle geduld, je voortdurende ondersteuning, jouw ideeën, enthousiasme en je (terecht)wijze(nde) woorden gedurende de bijna 6 1/2 jaar dat ik, door en door ’Ossi’, onder jouw begeleiding deze thesis mocht schrijven. Zonder jouw vertrouwen zou dit boek nooit naar de drukker zijn gegaan. Dank je wel! Christian, herzlichen Dank für die Leitung der Forschungsfahrt mit der Meteor, die Unterstützung und die vielen Tips während der vielen Besuche in Hamburg und der Projekt-Besprechungen. I would like to thank the reading committee for taking the time to read the thesis thoroughly and for the resulting suggestions which considerably improved the quality of this book. My sincerest thanks goes to