Difference between revisions of "Category:Lake Sediments Working Group"

Revision as of 17:15, 17 March 2017

Overview

In the Linked Earth context, a working group (WG) is a self-organized coalition of knowledgeable experts, whose activities are governed herewith. This page is dedicated to the discussion of data and metadata standards for lake sediments (see this page for a definition of the lake sediment archive), and aims to formulate a set of recommendations for such a standard. Note that chronological aspects should be discussed within the Chronologies WG.

Specific tasks

Thinking about data standards for lakes is a challenging task because of the incredible diversity of observations made on this archive. To start this process, the working group will focus on developing standards for the one variable in lake sediments that all scientists rely on: depth.

After we've done this process for depth, I suggest we reach out and broaden this group to include broad expertise of different sensor and observations types. A preliminary list is presented below.

Task 1: Depth

How should we report depth?

For this discussion we recommend:

• structuring discussions around what scientific questions one would want to ask of the data
• listing essential, recommended, and optional information for:
  • the measurements themselves
  • any inference made from the measurements (e.g. calibration to temperature)
  • the underlying uncertainties, and what those numbers correspond to (e.g. 1-sigma or 2-sigma?)
• provide an ideal data table for each type of observation, so the community knows what to report and how to report it.
• provide separate recommendations for new and legacy datasets

Initial thoughts on depth:

• We want to know both mid-point depth and thickness, or top and bottom depth.
  • Top and bottom depth is more explicit and self explanatory, but typically requires an additional step to use for analysis
  • Mid-point depth is more typically reported, and is what is needed for most age models, but can be ambiguous

• • I suggest we allow both, and recognizing that conversion is staightforward
• We need to distinguish between measured depth and modeled depth, in the cases where a composite depth scale is used.
• We need to ensure a common reference. I suggest that depth always refers to depth below lake floor.

Sensors

Sensors in lakes fall into several different categories

Sediment

Several observations can be made on sedimentary sensors including:

• grain size
• mineralogy
• geochemistry
• isotope geochemistry
• bulk organic carbon concentrations
• bulk inorganic carbon concentrations
• bulk nitrogen concentrations
• carbon to nitrogen ratios
• bulk organic carbon isotopic composition
• bulk inorganic carbon isotopic composition
• bulk nitrogen isotopic composition

Aquatic organisms

Several sensors may be found in lakes including Diatoms (may contribute microfossils) Ostracods (may contribute microfossils) Algae (may contribute biomarkers) Archaea (may contribute biomarkers) Bacteria (may contribute biomarkers) Fish (may contribute macrofossils)

Insects

Several sensors in the air above and around lakes may leave microfossils in lake sediments, these include - chironimid tests (microfossils)

Terrestrial plants

Plants growing around the lake and in the catchment of the lake may contribute macro and microfossils as well as biomarkers to the sediments. Plants are the sensors of the environment and the observations include: - pollen (microfossils) - leaf (macrofossils) - wood (macrofossils) - charchoal (macro or microfossils) - leaf wax n-alkanes (biomarkers) - leaf wax n-alkanoic acids (biomarkers) - leaf wax n-alkanols acids (biomarkers) - leaf wax terpenoids (biomarkers) - lignin (biomarkers)

Polls

Here are polls that the group might want to consider:

References