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Initial Core Descriptions
Introduction to making
physical observations and
documenting a stratigraphic
sequence
On the Cutting Edge-Teaching Climate
Change: Lessons from the Past
June 25, 2014 Lake E Teachers Workshop also at
http://lrc.geo.umn.edu/laccore/assets/pdf/sops/icd.pdf
Julie Brigham-Grette
UMass- Amherst
Why study lakes
• Lakes found in a variety of
environments
• Dynamic environmental systems
• Integrate environmental and climatic
change on a variety of time scales
• They collect sediments, organic matter
in response to their surroundings
• Sediments produce a continuous
archive of change; layer upon layer,
they record of Earth’s natural
experiments in change.
Earth Scientists – Time lords!
Sediment cores allow one to
understand past change and
system dynamics and to use this
information to improve
predictions about the future!
www.bbc.co.uk/doctorwho
Climate Today
Climate of Past
Climate Future
years
decades
centuries
Millennia
Today
Back in
Time
Lengthofcore Geochronology
• Age/Time
• Resolution
Learning Goals
• Concepts of the recent geologic record
– causality at a distance, cyclic causality, environmental
time delays
• How to describe sediments – standardized approach
to physical descriptions
– Photographic and written documentation
– Making observations and documenting those
observations in meaningful way
– Concept of particle size and sedimentary structures for
understanding depositional environments
– Facies model development
• Develop stratigraphic column, (Psicat)
• Quantitative image analysis (Image J)
Science Goals
 Difference between weather and
climate (ave of > 3 decades)
 Regional climate change vs global
climate change
The approach – lake sediments (Lake E example)
Proxies of climate  Modeling
and prediction of future change
today
Backintime
• Sedimentation rates and the geochronology of the core are
fundamental to understanding all of the physical properties and
quantifying the climate/environmental history. How can studies
of the sedimentology and sediment flux rates be used with other
proxies to best constrain the chronology?
• What are the hydrological, biological, and geochemical controls
on changes in sediment texture as they relate to changes in
climate?
• What are the lake processes and climatic conditions that produce
laminated, non-laminated and weakly laminated units throughout
the core?
Science questions should drive analysis
(ask students to develop their own)
ADD YOUR OWN QUESTIONS:
• How can the core stratigraphy be characterized into recognizable facies assemblages
related to changes in climate?
• What fundamental changes can we observe in the lake sedimentology .
• What processes cause these changes as they relate to climate history and landscape
change?
• Is there a fundamental change in the sediment properties and biogenic sedimentation
(or organic matter) with changes in land use, or external and internal forcing over
time?
• Characterization of primary controls on sediment character, flux rates and the
proportions of clastic vs. biogenic deposition
• Quantification of the relationship between sedimentology and climate change
(hydrology, lake ice cover history, terrestrial vs aquatic inputs etc.)
• Paleoclimate proxy development by comparisons between physical properties,
sedimentology, and scanned data sets.
Terms - learning the lingo
• Age resolution – years/cm
• Lithostratigraphy
– layering based on physical, lithic
properties and petrology
• Particle size/grain size
• Facies
– Sediments deposited in particular
environment or process ; a
vertical succession of facies
suggest lateral migration of the
depositional environment
• Laminae/varves
– Thin layers, if annual = varves
• Lets add more……..
Kurupa Lake core. Photo: Darrell Kaufman
Initial core splitting
Emi Ito photo
www.geotek.co.uk
Blades cut only the core
liner on either side.
Sediment is cut with SS
wire.
Split cores
Initial core splitting
Cheap and easy too – skill saw?
Using a Dremel Tool
Lake Sediment Core Processing Scheme
Example from ICDP Lake El‘gygytgyn Project
surface
cleaning
whole-core
magn. suscept.
(on site)
line scan pictures
with MSCL
susceptibility
and
color spectra
with SCLP3
1. line scan picture & surface relief
2. XRF light elements
with ITRAX core scanner
core description
manual
3. X-radiography
4. XRF heavy elements
with ITRAX core scanner
p-wave velocity
Gamma-ray density
magn. susceptibility
with MSCL
core archiving
LacCore Repository
Duluth, U.S.A.
core subsampling
Initial core scanning
• Magnetic susceptibility
• Line scan (continuous photography)
– Good digital camera can do!
• Gamma density
• Color Spectrometer
– L*a*b* parameters
– http://www.hunterlab.com/appnotes/an07_96a.pdf
• X-rays (use your local health clinic?)
• XRF scanning for major elements (ITRAX)
Geotek.co.uk
Filling out the
Barrel sheet –
what to look for,
what to describe
Texture (grain size)
Color (munsell scheme)
Unit thicknesses
nature of contacts
clast lithology
Compaction (stiffness)
sedimentary structures
organic content
fossils
Defining Facies
Making Smear slides
http://lrc.geo.umn.edu/laccor
e/assets/pdf/sops/sedclass_ba
sics.pdf
Sediment classification
• Macroscopic structure of the sediment –
– structures and textures (bedding features, texture, color)
• ID of major and minor components
– Eg. Clay, carbonate, peat, mud….)
1. Color + 2. Bedding + 3. Major Modifier + 4. Principal
Name + 5. Minor Constituents
e.g Dark reddish brown, massive, feldspathic clay with
carbonaceous debris and trace gastropod fragments
Schnurrenberger et al, 2003 at http://lrc.geo.umn.edu/laccore/assets/pdf/sops/sedclass.pdf
Classroom applications
• Grain size charts
http://www.concrete-
catalog.com/soil_compaction.html
Classroom applications
Munsell Color Book
Or Globe color book
http://en.wikipedia.org/wiki/Munsell_color_system
Smear Slides
Means of preparing a very thin
layer of unconsolidated material
embedded on a glass slide to
examine mineralogy, provenance,
grain shape, and identification of
microfossils, even tephras.
http://lrc.geo.umn.edu/laccore/assets/pdf/sops/smearslides.pdf
http://lrc.geo.umn.edu/laccore/assets/pdf/sops/smear_slide_basics.pdf
There is even a video tutorial !! AMY
ROCKS!https://tmi.laccore.umn.edu/tutorial/preparati
on
Vascular (terrestrial or aquatic)
organic matter
Quartz and/or feldspar, pitted and
stained with . . . something
Lake El’gygytgyn Facies – related to ice cover duration
Among other changes in lake system
Melles et al. 2010
Melles et al. 2012
Brigham-Grette et al. 2013
Glacial/cold warm Super warm
Objective is to define sediment facies
Paleolim 591L
Core Lithology-PG1351 Lake El’gygytgyn
Silty-Clastic Layer
Massive Grey Silty Clay Brownish-Grey Silty ClayOlive-Grey Laminae
Deposited under
anoxic conditions
i.e. Glacial-type
climate
Lithology
Depth(cm)
Unit
Olive-Grey
Silty Clay
Massive
Interglacial-type
sediments
UnitUnit
Sandy Layer
Depth: 385 cm
Transgressive – Regressive facies
With Lake level changes.
http://www.geol.umd.edu/~jmerck/geol342/lectures/16.html
Should develop a common language and
facies description
From mud to seeing fine laminae
Gravity Core GC-K05-03 Svalbard REU
1 yr?
L Poppick, Bates
Xrays done at
Umass Health Center
Lake E Pliocene and xrays
PSICAT – simple software for
constructing stratigraphic columns
http://portal.chronos.org/psicat-site/
PSICAT, CHRONOS's Paleontological
Stratigraphic Interval Construction and
Analysis Tool, is a stand-alone Java
based graphical editing tool for creating
and viewing stratigraphic column
diagrams from drill cores and outcrops.
It is customized to the task of working
with stratigraphic columns and captures
data digitally as you draw and edit the
diagram.
Initial developed by Josh Reed for ANDRILL Project.
`
1pm Awesome WOW! 2PM, better than 1PM 3 PM 4pm classy group
PSICAT Stratigraphic Log Summary
File  Export Summary Spreadsheet
Image J – simple analysis software
http://rsbweb.nih.gov/ij/
• Allows simple or complex
analysis of textures, layering,
color
• Runs on any platform, public
domain
• Allows statistics, histograms
and surface profiles to transfer
to excel.
Use your own
core images or
have students
examine cores
accessible at
CoreRef.org
289.00 m comp depth
10 cm
Image J analysis of Lake El’gygytgyn thin section
without any enhancements to default settings.
Main Facies
• Interglacial
– Non-laminated
– Lower TOC
– High Magnetic susceptibility (MS)
– Median Grain-size = 3.5 µm
• Glacial
– Finely Laminated
– “Bleb” Structures
– Higher TOC, low MS
– Authigenic minerals
– Median Grain-size = 3.5 µm
Detailed Sedimentology via Image Analysis (Francus and Asikainen)
http://www.geo.umass.edu/climate/francus/ss1_slide_show.htm
SEM view
SEM view
On-line Data Archiving and Global Access

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Initial core descript teachers

  • 1. Initial Core Descriptions Introduction to making physical observations and documenting a stratigraphic sequence On the Cutting Edge-Teaching Climate Change: Lessons from the Past June 25, 2014 Lake E Teachers Workshop also at http://lrc.geo.umn.edu/laccore/assets/pdf/sops/icd.pdf Julie Brigham-Grette UMass- Amherst
  • 2. Why study lakes • Lakes found in a variety of environments • Dynamic environmental systems • Integrate environmental and climatic change on a variety of time scales • They collect sediments, organic matter in response to their surroundings • Sediments produce a continuous archive of change; layer upon layer, they record of Earth’s natural experiments in change.
  • 3. Earth Scientists – Time lords! Sediment cores allow one to understand past change and system dynamics and to use this information to improve predictions about the future! www.bbc.co.uk/doctorwho Climate Today Climate of Past Climate Future
  • 5. Learning Goals • Concepts of the recent geologic record – causality at a distance, cyclic causality, environmental time delays • How to describe sediments – standardized approach to physical descriptions – Photographic and written documentation – Making observations and documenting those observations in meaningful way – Concept of particle size and sedimentary structures for understanding depositional environments – Facies model development • Develop stratigraphic column, (Psicat) • Quantitative image analysis (Image J)
  • 6. Science Goals  Difference between weather and climate (ave of > 3 decades)  Regional climate change vs global climate change
  • 7. The approach – lake sediments (Lake E example)
  • 8. Proxies of climate  Modeling and prediction of future change today Backintime
  • 9. • Sedimentation rates and the geochronology of the core are fundamental to understanding all of the physical properties and quantifying the climate/environmental history. How can studies of the sedimentology and sediment flux rates be used with other proxies to best constrain the chronology? • What are the hydrological, biological, and geochemical controls on changes in sediment texture as they relate to changes in climate? • What are the lake processes and climatic conditions that produce laminated, non-laminated and weakly laminated units throughout the core? Science questions should drive analysis (ask students to develop their own)
  • 10. ADD YOUR OWN QUESTIONS: • How can the core stratigraphy be characterized into recognizable facies assemblages related to changes in climate? • What fundamental changes can we observe in the lake sedimentology . • What processes cause these changes as they relate to climate history and landscape change? • Is there a fundamental change in the sediment properties and biogenic sedimentation (or organic matter) with changes in land use, or external and internal forcing over time? • Characterization of primary controls on sediment character, flux rates and the proportions of clastic vs. biogenic deposition • Quantification of the relationship between sedimentology and climate change (hydrology, lake ice cover history, terrestrial vs aquatic inputs etc.) • Paleoclimate proxy development by comparisons between physical properties, sedimentology, and scanned data sets.
  • 11. Terms - learning the lingo • Age resolution – years/cm • Lithostratigraphy – layering based on physical, lithic properties and petrology • Particle size/grain size • Facies – Sediments deposited in particular environment or process ; a vertical succession of facies suggest lateral migration of the depositional environment • Laminae/varves – Thin layers, if annual = varves • Lets add more…….. Kurupa Lake core. Photo: Darrell Kaufman
  • 12. Initial core splitting Emi Ito photo www.geotek.co.uk
  • 13. Blades cut only the core liner on either side. Sediment is cut with SS wire. Split cores Initial core splitting
  • 14. Cheap and easy too – skill saw? Using a Dremel Tool
  • 15. Lake Sediment Core Processing Scheme Example from ICDP Lake El‘gygytgyn Project surface cleaning whole-core magn. suscept. (on site) line scan pictures with MSCL susceptibility and color spectra with SCLP3 1. line scan picture & surface relief 2. XRF light elements with ITRAX core scanner core description manual 3. X-radiography 4. XRF heavy elements with ITRAX core scanner p-wave velocity Gamma-ray density magn. susceptibility with MSCL core archiving LacCore Repository Duluth, U.S.A. core subsampling
  • 16. Initial core scanning • Magnetic susceptibility • Line scan (continuous photography) – Good digital camera can do! • Gamma density • Color Spectrometer – L*a*b* parameters – http://www.hunterlab.com/appnotes/an07_96a.pdf • X-rays (use your local health clinic?) • XRF scanning for major elements (ITRAX) Geotek.co.uk
  • 17. Filling out the Barrel sheet – what to look for, what to describe Texture (grain size) Color (munsell scheme) Unit thicknesses nature of contacts clast lithology Compaction (stiffness) sedimentary structures organic content fossils Defining Facies Making Smear slides http://lrc.geo.umn.edu/laccor e/assets/pdf/sops/sedclass_ba sics.pdf
  • 18. Sediment classification • Macroscopic structure of the sediment – – structures and textures (bedding features, texture, color) • ID of major and minor components – Eg. Clay, carbonate, peat, mud….) 1. Color + 2. Bedding + 3. Major Modifier + 4. Principal Name + 5. Minor Constituents e.g Dark reddish brown, massive, feldspathic clay with carbonaceous debris and trace gastropod fragments Schnurrenberger et al, 2003 at http://lrc.geo.umn.edu/laccore/assets/pdf/sops/sedclass.pdf
  • 19. Classroom applications • Grain size charts http://www.concrete- catalog.com/soil_compaction.html
  • 20. Classroom applications Munsell Color Book Or Globe color book http://en.wikipedia.org/wiki/Munsell_color_system
  • 21. Smear Slides Means of preparing a very thin layer of unconsolidated material embedded on a glass slide to examine mineralogy, provenance, grain shape, and identification of microfossils, even tephras. http://lrc.geo.umn.edu/laccore/assets/pdf/sops/smearslides.pdf http://lrc.geo.umn.edu/laccore/assets/pdf/sops/smear_slide_basics.pdf There is even a video tutorial !! AMY ROCKS!https://tmi.laccore.umn.edu/tutorial/preparati on Vascular (terrestrial or aquatic) organic matter Quartz and/or feldspar, pitted and stained with . . . something
  • 22. Lake El’gygytgyn Facies – related to ice cover duration Among other changes in lake system Melles et al. 2010 Melles et al. 2012 Brigham-Grette et al. 2013 Glacial/cold warm Super warm Objective is to define sediment facies
  • 23. Paleolim 591L Core Lithology-PG1351 Lake El’gygytgyn Silty-Clastic Layer Massive Grey Silty Clay Brownish-Grey Silty ClayOlive-Grey Laminae Deposited under anoxic conditions i.e. Glacial-type climate Lithology Depth(cm) Unit Olive-Grey Silty Clay Massive Interglacial-type sediments UnitUnit Sandy Layer Depth: 385 cm
  • 24. Transgressive – Regressive facies With Lake level changes. http://www.geol.umd.edu/~jmerck/geol342/lectures/16.html
  • 25. Should develop a common language and facies description
  • 26. From mud to seeing fine laminae Gravity Core GC-K05-03 Svalbard REU
  • 27.
  • 28. 1 yr? L Poppick, Bates Xrays done at Umass Health Center Lake E Pliocene and xrays
  • 29. PSICAT – simple software for constructing stratigraphic columns http://portal.chronos.org/psicat-site/ PSICAT, CHRONOS's Paleontological Stratigraphic Interval Construction and Analysis Tool, is a stand-alone Java based graphical editing tool for creating and viewing stratigraphic column diagrams from drill cores and outcrops. It is customized to the task of working with stratigraphic columns and captures data digitally as you draw and edit the diagram. Initial developed by Josh Reed for ANDRILL Project.
  • 30. ` 1pm Awesome WOW! 2PM, better than 1PM 3 PM 4pm classy group PSICAT Stratigraphic Log Summary
  • 31. File  Export Summary Spreadsheet
  • 32. Image J – simple analysis software http://rsbweb.nih.gov/ij/ • Allows simple or complex analysis of textures, layering, color • Runs on any platform, public domain • Allows statistics, histograms and surface profiles to transfer to excel. Use your own core images or have students examine cores accessible at CoreRef.org
  • 33. 289.00 m comp depth 10 cm
  • 34. Image J analysis of Lake El’gygytgyn thin section without any enhancements to default settings.
  • 35. Main Facies • Interglacial – Non-laminated – Lower TOC – High Magnetic susceptibility (MS) – Median Grain-size = 3.5 µm • Glacial – Finely Laminated – “Bleb” Structures – Higher TOC, low MS – Authigenic minerals – Median Grain-size = 3.5 µm Detailed Sedimentology via Image Analysis (Francus and Asikainen) http://www.geo.umass.edu/climate/francus/ss1_slide_show.htm
  • 38. On-line Data Archiving and Global Access

Editor's Notes

  1. From Mud to wiggles!
  2. Samuel Taylor Coleridge was an English poet, critic, and philosopher who was, along with his friend William Wordsworth, one of the founders of the Romantic Movement in England and one of the Lake Poets. He is probably best known for his poems The Rime of the Ancient Mariner and Kubla Khan, as well as his major prose work Biographia Literaria.
  3. Most people do not understand geologic time.
  4. Grotzer, T., and Bell, B., 2004, How does grasping the underlying casual structures of ecosystems impact students' understanding? J. Bio. Educ., 38, 16-29.
  5. Add definitions of color