1. Physical Controls on Carbonate Intraclasts: Modern Flat Pebbles From Great Salt Lake, Utah.
- Author
-
Smith, B. P., Ingalls, M., Trower, E. J., Lingappa, U. F., Present, T. M., Magyar, J. S., and Fischer, W. W.
- Subjects
BIOTURBATION ,TOPOGRAPHY ,GEOPHYSICS ,HYPOTHESIS ,SEAWATER - Abstract
In carbonate‐forming environments, authigenic minerals can cement surface sediments into centimeter‐sized intraclasts that are later reworked into "flat‐pebble" or "edgewise" conglomerates. Flat‐pebble conglomerates comprise only a small portion of facies in modern marine environments but are common in ancient strata, implying that seafloor cements were more widespread in the past. Flat‐pebble conglomerates nearly disappeared after the Ordovician radiation, yet it is unclear if this decline was due to changing seawater chemistry or if increased infaunalization and bioturbation simply worked to break down nascent clasts. We discovered a process analog that produces flat‐pebble conglomerates around the Great Salt Lake, Utah, USA, and studied these facies using field observations, wave models, satellite imagery, petrography, and microanalytic chemical data. Clasts were sourced from wave‐rippled grainstone that cemented in situ in offshore environments. Lake floor cements formed under aragonite saturation states that are lower than modern marine settings, suggesting that physical processes are at least as important as chemical ones. Results from our wave models showed that coarse sediments near the field site experience quiescent periods of up to 6 months between suspension events, allowing isopachous cements to form. Using a simple mathematical framework, we show that the main difference between Great Salt Lake and modern, low‐energy marine settings is that the latter has enough bioturbating organisms to break up clasts. Observations from Great Salt Lake demonstrate how geologic trends in flat‐pebble abundance could largely reflect changes in total infaunal biomass and ecology without requiring regional‐to‐global changes in seawater chemistry. Plain Language Summary: Calcium carbonate is a common sedimentary mineral that precipitates quickly under Earth surface conditions. If carbonate sediments are at rest for long periods of time, they may solidify via cementation into flat, pebble‐sized clasts. Geologic trends show that flat pebbles are anticorrelated with burrows, suggesting they may tell us about animal evolution and ecology. However, it was unknown if animals disrupt clasts through chemical means, leading to slower rates of mineral growth, or if they physically push sediments apart, breaking up nascent cements. We studied flat pebbles forming in Great Salt Lake, Utah, where the water is too salty for burrowing animals. The composition of lake water should lead to slower growth rates for carbonate minerals, yet clasts still form. We conclude that pebbles form during quiescent intervals with little physical energy to move grains, either from waves or from burrowing organisms. As a result, ancient flat pebbles are probably not unique markers for seawater chemistry. Key Points: Sediment cohesion within carbonate environments depends on both physical and chemical energy near the sediment‐water interfaceIf sediment transport is infrequent, burrowing animals provide a significant source of physical energySubstrate cohesion may record physical changes related to the number and behavior of animals rather than geochemical conditions [ABSTRACT FROM AUTHOR]
- Published
- 2020
- Full Text
- View/download PDF