Paper out in Geology

THIS POST CAN BE FOUND AT NEW BLOG, CALLED CLASTIC DETRITUS, HERE

A paper i'm a co-author on is in the September edition of Geology. I'm swamped right now and don't have time to write a coherent post about it....but I will soon.

In the meantime, check it out (if you have access, of course):

Highstand fans in the California borderland: The overlooked deep-water depositional systems
Jacob A. Covault, William R. Normark, Brian W. Romans, and Stephan A. Graham

Sediment accumulation rates and bias: The Sadler effect

A key element to understanding sediment flux is the determination of accumulation rates in areas of net deposition. How fast (or slow) is sediment piling up? How is that rate distributed in space? How does it change over time? What does it tell us about the controls of sediment flux?

Sweet. This is simple. Just measure the thickness of sediment (or sedimentary rock), divide by the duration, and interpret! Well...it turns out it's not so simple after all.

This post is a little bit about a very important paper that I don't see cited enough.

Sadler, P.M., 1981, Sediment accumulation rates and the completeness of stratigraphic sections: Journal of Geology, v. 89.

The main gist of the paper is summarized nicely in the first statements of the abstract:

"A compilation of nearly 25,000 rates of sediment accumulation shows that they are extremely variable, spanning at least 11 orders of magnitude. Much of this variation results from compiling rates determined for different time spans: there is a systematic trend of falling mean rate with increasing time span."

In other words, the longer the time interval measured the lower the sedimentation rate. The image below is Sadler's Figure 1 with some of my scribblings on it. It is a log-log plot of sedimentation rate (meters per 1000 years) on the vertical axis and timespan (years) and thickness (meters) on the lower and upper horizontal axes, respectively. For now just focus on the 'a' figure...the one on the left. And also don't worry about the Roman numerals (i, ii, etc.).


The trend is pretty obvious. The data in the upper left have very high sedimentation rates, were measured over very short time intervals (hours to months), and are relatively thin. The area to the lower right represents sedimentation rates several orders of magnitude slower and have measured time intervals in the millions to 10s of millions of years. There's some spread in the data of course, but in general this is a robust trend. What is underlying this relationship?

The tendency for sediment to compact as it buried (and thus be thinner) is a contribution but does not account for the bulk of the relationship. What you are seeing here is essentially the nature of sedimentation. It is discontinuous and highly spasmodic. In most depositional environments, the duration of actual deposition of sediment is very small compared to the time the system sits there doing little to nothing. I think Derek Ager said the history of sedimentation is like being in the military....hours of boredom separated by brief moments of terror.

So, we are seeing the effect of including more time of non-deposition (i.e., nothing happening) as we increase the span of the measured time interval. But wait...there's more! We are also seeing the nature of sediment preservation over geologic time scales. That is, the farther back into time we go, the more time of erosion is included (remember, these systems are net-depositional...there is some erosion occurring). The younger the section, the more "complete" it tends to be. Sadler discusses this issue of preservation and stratigraphic completeness very elegantly with this statement:

"Sedimentary sequences...record the passage of geological time as an alternating set of sedimentary increments and gaps. The ratio of these two components is stratigraphic completeness."

Sadler certainly was not the first to recognize this (another famous paper by Barrell, which I will post about someday, is notable for discussing completeness back in 1917) but this paper was the first to quantify it. A sizeable chunk of the paper goes through methods for calculating completeness.

Several recent studies, including the pioneering paper by Molnar & England (1990), discuss the apparent increase in sedimentation rate observed in the last 20-30 million years. This has led to countless discussions about whether this signature is recording changing uplift rates or changing climate. Now of course we shan't attribute this trend solely to Sadler's measurement interval bias, because there very well may be an actual increase in rate. But, the point of this post is to highlight Sadler's work and how we shouldn't forget about it. Many of these papers do not even mention it. Sampling bias as a result for a study is not very exciting and probably won't result in the cover of Nature or Science, but if we are to adequately deconvolve all the factors at play we need to remember biases like this.

Molnar, P., and England, P., 1990, Late Cenozoic uplift of mountain ranges and global climte change: chicken or egg? Nature, v. 346.

Sediment Flux and Luggage Carousels

Research that I have been doing recently involves the study of sediment flux. That is, what is the history, the temporal distribution, of the erosion, transport, and deposition of sediment. From the erosion of a particle in the uplands, into a river system, perhaps spending some time in a coastal system, and then into a deep marine basin. I've been looking at a temporal scale of hundreds to thousands of years, but one could examine this at a scale of millions of years. Of course, the farther back into Earth history, the lower the resolution. Moreover, the farther back in Earth history, the more fragmented is the contextual information about the system. Investigating sediment flux requires a lot of context

The ultimate question is, of course: what are the controls on sediment flux? Can we deconvolve interacting factors including, but not limited to:

• climate (e.g., increased precipitation leading to increased runoff/streamflow)
  
• sea-level stands (e.g., lowstands of sea level during glacial maxima)
  
• tectonic movements (e.g., increased uplift rate of sediment source area leading to increased erosion rate)
• intrinsic behavior of the sedimentary system (e.g., meandering of a river, migration of dunes and other bedforms, distributive patterns, etc.)

This is what I spend my time pondering. Earlier today I was standing at the luggage carousel in the airport. Everybody stands there staring at the mouth of the conveyor from where their bag (hopefully) appears. We stand there and wonder what controls the order, why the delivery of bags come in clusters, and other nonsense....essentially, we are wondering what is controlling the flux of luggage. Well, maybe only I wonder this.....anyway, all we have to do to figure this out is simply observe what is happening on the other side of the luggage delivery system.

I don't really care about luggage delivery systems...I just want my bag. But I do care about sedimentary systems. It's definitely more complex than the carousel too. In the coming weeks I am going to post more about this area of my research. Check out a post from February in the meantime.

Image at top of Santa Ynez Creek, California; from Jon Warrick's work