Reconstruction of Ediacaran to Early Cambrian ocean pH and weathering conditions

This dissertation deals with the reconstruction of ocean pH conditions and the quantification of weathering rates by boron and strontium isotope analyses on Ediacaran and Early Cambrian marine carbonate rocks. In order to compare local signals and specific features with global patterns, a variety of...

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Bibliographic Details
Main Author: Ohnemüller, Frank
Other Authors: Kasemann, Simone A., Prave, Anthony
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Universität Bremen 2014
Subjects:
550
Online Access:https://media.suub.uni-bremen.de/handle/elib/716
https://nbn-resolving.org/urn:nbn:de:gbv:46-00103948-13
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spelling ftsubbremen:oai:media.suub.uni-bremen.de:Publications/elib/716 2023-05-15T17:50:17+02:00 Reconstruction of Ediacaran to Early Cambrian ocean pH and weathering conditions Rekonstruktion der Meerwasser pH-Werte und Verwitterungsbedingungen im Ediacarium und Frühen Kambrium Ohnemüller, Frank Kasemann, Simone A. Prave, Anthony 2014-08-08 application/pdf https://media.suub.uni-bremen.de/handle/elib/716 https://nbn-resolving.org/urn:nbn:de:gbv:46-00103948-13 eng eng Universität Bremen FB5 Geowissenschaften https://media.suub.uni-bremen.de/handle/elib/716 urn:nbn:de:gbv:46-00103948-13 info:eu-repo/semantics/openAccess Bitte wählen Sie eine Lizenz aus: (Unsere Empfehlung: CC-BY) CC-BY ocean pH weathering reconstruction boron strontium Cambrian Ediacaran PCC boundary ocean acidification Marinoan 550 550 Earth sciences and geology ddc:550 Dissertation doctoralThesis 2014 ftsubbremen 2022-11-09T07:09:26Z This dissertation deals with the reconstruction of ocean pH conditions and the quantification of weathering rates by boron and strontium isotope analyses on Ediacaran and Early Cambrian marine carbonate rocks. In order to compare local signals and specific features with global patterns, a variety of sections on two different palaeo continents (China, Kazakhstan) were examined and compared to data from the Namibian Congo craton. The entire Ediacaran and Early Cambrian was characterized by minor to major ocean pH fluctuations and a general increase in weathering rates and fluxes to the ocean. Ocean acidification events are indicated for the aftermath of the Marinoan glaciation as well as for the Precambrian-Cambrian boundary. The changes in ocean pH and weathering rates had a significant influence on ocean geochemistry and may have decisively contributed to the creation of new ecological niches, possibly enabling the appearance of multicellular animals and reinforcing their radiation. Doctoral or Postdoctoral Thesis Ocean acidification Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen)
institution Open Polar
collection Media SuUB Bremen (Staats- und Universitätsbibliothek Bremen)
op_collection_id ftsubbremen
language English
topic ocean pH
weathering
reconstruction
boron
strontium
Cambrian
Ediacaran
PCC boundary
ocean acidification
Marinoan
550
550 Earth sciences and geology
ddc:550
spellingShingle ocean pH
weathering
reconstruction
boron
strontium
Cambrian
Ediacaran
PCC boundary
ocean acidification
Marinoan
550
550 Earth sciences and geology
ddc:550
Ohnemüller, Frank
Reconstruction of Ediacaran to Early Cambrian ocean pH and weathering conditions
topic_facet ocean pH
weathering
reconstruction
boron
strontium
Cambrian
Ediacaran
PCC boundary
ocean acidification
Marinoan
550
550 Earth sciences and geology
ddc:550
description This dissertation deals with the reconstruction of ocean pH conditions and the quantification of weathering rates by boron and strontium isotope analyses on Ediacaran and Early Cambrian marine carbonate rocks. In order to compare local signals and specific features with global patterns, a variety of sections on two different palaeo continents (China, Kazakhstan) were examined and compared to data from the Namibian Congo craton. The entire Ediacaran and Early Cambrian was characterized by minor to major ocean pH fluctuations and a general increase in weathering rates and fluxes to the ocean. Ocean acidification events are indicated for the aftermath of the Marinoan glaciation as well as for the Precambrian-Cambrian boundary. The changes in ocean pH and weathering rates had a significant influence on ocean geochemistry and may have decisively contributed to the creation of new ecological niches, possibly enabling the appearance of multicellular animals and reinforcing their radiation.
author2 Kasemann, Simone A.
Prave, Anthony
format Doctoral or Postdoctoral Thesis
author Ohnemüller, Frank
author_facet Ohnemüller, Frank
author_sort Ohnemüller, Frank
title Reconstruction of Ediacaran to Early Cambrian ocean pH and weathering conditions
title_short Reconstruction of Ediacaran to Early Cambrian ocean pH and weathering conditions
title_full Reconstruction of Ediacaran to Early Cambrian ocean pH and weathering conditions
title_fullStr Reconstruction of Ediacaran to Early Cambrian ocean pH and weathering conditions
title_full_unstemmed Reconstruction of Ediacaran to Early Cambrian ocean pH and weathering conditions
title_sort reconstruction of ediacaran to early cambrian ocean ph and weathering conditions
publisher Universität Bremen
publishDate 2014
url https://media.suub.uni-bremen.de/handle/elib/716
https://nbn-resolving.org/urn:nbn:de:gbv:46-00103948-13
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://media.suub.uni-bremen.de/handle/elib/716
urn:nbn:de:gbv:46-00103948-13
op_rights info:eu-repo/semantics/openAccess
Bitte wählen Sie eine Lizenz aus: (Unsere Empfehlung: CC-BY)
op_rightsnorm CC-BY
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