The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation
The Caribbean carbonate crash was a time of increased regional carbonate dissolution at the middle to late Miocene transition. It is marked by five dissolution episodes, occurring from 12-10 Ma, characterized by significant reductions in carbonate mass accumulation rates (CO$\sb3$ MAR). We determine...
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ftriceuniv:oai:scholarship.rice.edu:1911/17317 2023-05-15T13:34:53+02:00 The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation Roth, Joy Michele Droxler, Andre W. 1999 135 p. application/pdf https://hdl.handle.net/1911/17317 eng eng Roth, Joy Michele. "The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation." (1999) Master’s Thesis, Rice University. https://hdl.handle.net/1911/17317 . https://hdl.handle.net/1911/17317 THESIS GEOL. 1999 ROTH Geology Physical oceanography Geochemistry Thesis Text 1999 ftriceuniv 2022-08-09T20:50:53Z The Caribbean carbonate crash was a time of increased regional carbonate dissolution at the middle to late Miocene transition. It is marked by five dissolution episodes, occurring from 12-10 Ma, characterized by significant reductions in carbonate mass accumulation rates (CO$\sb3$ MAR). We determined carbonate content and CO$\sb3$ MAR for sites 998-1000 over the middle to late Miocene interval. Stable isotope composition of benthic foraminifers is used to track changes in deep water masses. Carbonate mineralogies are determined for the shallow site 1000 (927 m water depth) to detect dissolution of metastable carbonates at sub-thermocline depths. The geochemical changes during the carbonate period are similar to those that occur during the Caribbean Quaternary interglacial stages, times when Antarctic Intermediate Water (AAIW) filled the Caribbean to abyssal depths. The initiation of North Atlantic Deep Water (NADW) production during this period, possibly caused by the partial closing of the Isthmus of Panama and the opening of Pedro Channel (northern Nicaragua Rise), led to reorganization of global thermohaline circulation. The increase of return flow that passes through the Caribbean may have brought corrosive AAIW into the Caribbean, causing dissolution of carbonate sediment at the sea floor. Thesis Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic Rice University: Digital Scholarship Archive Antarctic |
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Rice University: Digital Scholarship Archive |
op_collection_id |
ftriceuniv |
language |
English |
topic |
Geology Physical oceanography Geochemistry |
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Geology Physical oceanography Geochemistry Roth, Joy Michele The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation |
topic_facet |
Geology Physical oceanography Geochemistry |
description |
The Caribbean carbonate crash was a time of increased regional carbonate dissolution at the middle to late Miocene transition. It is marked by five dissolution episodes, occurring from 12-10 Ma, characterized by significant reductions in carbonate mass accumulation rates (CO$\sb3$ MAR). We determined carbonate content and CO$\sb3$ MAR for sites 998-1000 over the middle to late Miocene interval. Stable isotope composition of benthic foraminifers is used to track changes in deep water masses. Carbonate mineralogies are determined for the shallow site 1000 (927 m water depth) to detect dissolution of metastable carbonates at sub-thermocline depths. The geochemical changes during the carbonate period are similar to those that occur during the Caribbean Quaternary interglacial stages, times when Antarctic Intermediate Water (AAIW) filled the Caribbean to abyssal depths. The initiation of North Atlantic Deep Water (NADW) production during this period, possibly caused by the partial closing of the Isthmus of Panama and the opening of Pedro Channel (northern Nicaragua Rise), led to reorganization of global thermohaline circulation. The increase of return flow that passes through the Caribbean may have brought corrosive AAIW into the Caribbean, causing dissolution of carbonate sediment at the sea floor. |
author2 |
Droxler, Andre W. |
format |
Thesis |
author |
Roth, Joy Michele |
author_facet |
Roth, Joy Michele |
author_sort |
Roth, Joy Michele |
title |
The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation |
title_short |
The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation |
title_full |
The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation |
title_fullStr |
The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation |
title_full_unstemmed |
The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation |
title_sort |
caribbean carbonate crash at the middle to late miocene transition and the establishment of the modern global thermohaline circulation |
publishDate |
1999 |
url |
https://hdl.handle.net/1911/17317 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic |
genre_facet |
Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic |
op_relation |
Roth, Joy Michele. "The Caribbean carbonate crash at the middle to late Miocene transition and the establishment of the modern global thermohaline circulation." (1999) Master’s Thesis, Rice University. https://hdl.handle.net/1911/17317 . https://hdl.handle.net/1911/17317 THESIS GEOL. 1999 ROTH |
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1766058865401528320 |