dc.contributor.author
Hodgson, David M.
dc.contributor.author
Bernhardt, Anne
dc.contributor.author
Clare, Michael A.
dc.contributor.author
Da Silva, Anne-Christine
dc.contributor.author
Fosdick, Julie C.
dc.contributor.author
Mauz, Barbara
dc.contributor.author
Midtkandal, Ivar
dc.contributor.author
Owen, Amanda
dc.contributor.author
Romans, Brian W.
dc.date.accessioned
2018-11-16T13:44:10Z
dc.date.available
2018-11-16T13:44:10Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/23215
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-1007
dc.description.abstract
The 7.6 billion people living on our planet face a number of pressing issues that include climate change, food and energy security, natural resource management, human health, clean water management, sustainable use of the oceans, building resilient infrastructure, and responsible production and consumption (UNSDGs, 2015). Many of these issues involve a better understanding of ancient, modern, and future process interactions at and below the Earth's surface. Particulate transport processes and fluxes are the key physical measures, and sedimentary successions form the critical archives, which permit investigations into the response of the planet's interconnected systems to climate change, and the triggers, magnitudes, and frequency of natural hazards. Advances in quantification and forecasting of particulate and pollutant transport across the land, the continental shelf, and in the deep-ocean are urgently required to improve societal resilience to these planetary changes and hazards. Given the lack of long-term (>100s of years) instrumental records and uncertainties in future Earth system behavior, analysis of both recent and ancient sedimentary archives is required to tackle these challenges. A number of questions arise when faced with attempting such reconstructions from depositional sequences. For instance, can we confidently attribute processes to the resultant sedimentary deposits? How can we establish a precise chronology for past events? How did past events respond to environmental controls? How complete are sedimentary sequences? What post-depositional processes may complicate their interpretation?
[...]
en
dc.format.extent
9 Seiten
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
dc.subject
sedimentology
en
dc.subject
stratigraphy
en
dc.subject
source-to-sink
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::550 Geowissenschaften, Geologie::551 Geologie, Hydrologie, Meteorologie
dc.title
Grand Challenges (and Great Opportunities) in Sedimentology, Stratigraphy, and Diagenesis Research
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation.articlenumber
173
dcterms.bibliographicCitation.doi
10.3389/feart.2018.00173
dcterms.bibliographicCitation.journaltitle
Frontiers in Earth Science
dcterms.bibliographicCitation.volume
6
dcterms.bibliographicCitation.url
https://www.frontiersin.org/articles/10.3389/feart.2018.00173/full
refubium.affiliation
Geowissenschaften
refubium.affiliation.other
Institut für Geologische Wissenschaften
refubium.note.author
Der Artikel wurde in einer reinen Open-Access-Zeitschrift publiziert.
refubium.resourceType.isindependentpub
no
dcterms.accessRights.openaire
open access
dcterms.isPartOf.issn
2296-6463