Video recording of “Forest restoration theory and practice based on Indigenous cultural tending”

Here a Youtube video of my recent lecture and discussion in the course FORESTS, hosted by the Humanities Center of Texas Tech University. Many thanks to Bruce Clarke and Michael Borshuk for facilitating this talk!

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Scientific meeting on Gaia at the Geological Society of London – November 11, 2015

Carlsbad caverns. Photo by Lee Klinger.

On November 11, 2015 there will be a meeting entitled “Puzzle of Earth’s Uninterrupted Habitability” to be held at the Geological Society of London (GSL). This meeting will have a strong emphasis on Gaia theory and several prominent Gaian scholars will be speaking, including Tim Lenton, David Wilkinson, Toby Tyrrell, and David Schwartzman. As a Fellow of the GSL I have been invited to speak at this meeting. Here are the title and abstract of my talk:

“Biological mediation of acidity and alkalinity: Does habitability require regulation of environmental pH?”

Lee Klinger, Independent Scientist, Big Sur, CA USA

Abstract – Climatic cycles such as ice ages represent large excursions in global temperatures and are associated with significant changes in atmospheric CO2, non-sea salt sulfate, and dust, as recorded in ice cores. Ice age excursions in the pH of marine waters are predicted to result from the altered concentrations of CO2 in those waters. In addition, there are a number of biologically mediated processes affecting the pH of terrestrial and marine environments.

During interglacials terrestrial ecosystems are dominated by forests and grasslands that experience frequent disturbances, especially fire, which tends to alkalinize the soils. At the onset of glaciation higher latitude fire regimes subside and the forests become podzolized, with a corresponding decrease in soil pH. Many of these areas are eventually paludified, owing primarily to the acidifying and swamping effects of mosses and lichens, which eventually dominate the expanding peatlands. Mosses and lichens are known to stimulate silicate weathering rates to levels that could significantly reduce atmospheric CO2, and the cooling effects of peatlands are thought to play a role in ice age initiation. There is evidence that the production of iron-rich organic acids by peatlands greatly enhances phytoplankton blooms in adjacent coastal areas. Rainfall chemistry from the Pacific northwest points to the occurrence of biogenic acid rain likely originating from DMS and other biogenic sulfur compounds emitted by the phytoplankton. A feedback results through the nss-sulfate deposition enhancing the growth of mosses.

As ice ages progress and glaciers grow, dust levels in the atmosphere are also seen to rise. Much of this dust is due to an increase in glacial loess. The iron content of the dust stimulates marine productivity in open ocean areas. Oceanic inputs of iron from volcanic ash and glacial outwash are also seen to increase during glacial periods.

The culmination of the glacial period is defined by feedbacks involving the expansion of glaciers into areas formerly occupied by peatlands. The high mineral content of the glacial loess, along with episodes of volcanic ash would tend to alkalinize the terrestrial ecosystems and discourage the proliferation of mosses and other acidifying organisms.

Thus, the pH excursions in the ice age cycle may be related to the biogeochemical coupling of the iron and sulfur cycles. This coupling could have its roots in the Precambrian banded iron formations (BIFs), cyclic depositions of iron-rich minerals that are likely biogenic in origin. BIFs are seen to be closely associated with snowball earth conditions.

Life and the Planet – Part 2

Lynn Margulis, who as Lovelock said earlier “put the flesh and bones” on Gaia, spoke on ‘Evolutionary novelty in the Proterozoic eon: Symbiogenesis in Gaia’. She described a sequence of evolutionary events involving eubacteria and thermobacteria coming together to form the first eukaryotes. This occurred not through random mutations but through symbiosis occurring over evolutionary time scales, or symbiogenesis. While Lynn is often credited with the theory of symbiogenesis she emphatically states that others preceded her in this idea, particular a Russian scientist, Boris Mikhaylovich Kozo-Polyansky, who in 1924 published a book “Symbiogenesis: A New Principle in Evolution”. Still, Lynn undoubtedly put the “flesh and bones” on the theory of Symbiogenesis as well.

Nicholas Butterfield spoke on ‘Multicellularity in deep time’ where he described the early fossil record of various multicellular life forms. He pointed out that by ~1 Ga ago there is evidence for clonal colonies of cyanobacteria, coenobial and filamentous green algae, and branched multicellular filaments of red algae. There is even a 850 Ma old fungus-like fossil with complex multicellular vesicles/hyphae. He states, however, that at this time there is “not a whisper of land plant fossils”. Doubting that this is a preservation issue, he left open the question of plant and animal life on land in the Proterozoic.

Speaking on ‘Neoproterozoic glaciation: Microbes at work in terrestrial oases’ Ian Fairchild acknowledged that even under the most extreme conditions of Snowball Earth life must have persisted and even flourished in places. He described stratigraphic sequences from northern Svalbard which bear units of sandstone, rhythmites, and carbonates which appear to owe their origin, in part, to microbial mats of cyanobacteria. He concludes that “extremophile” life flourished at this time and provided a geochemical record of the Cryogenian (Snowball Earth) period. Unfortunately, he offered no ideas on possible biological feedbacks on the climate.

The potential role of peatland dynamics in ice-age initiation

As I mentioned in a previous post I am putting up some of my earlier work on feedback mechanisms by which the planet cools itself. This background will be useful in an upcoming post on planetary temperature regulation.

The potential role of peatland dynamics in ice-age initiation

by Lee F. Klinger, John A. Taylor, & Lars G. Franzen

Quaternary Research 45: 89-92 (1996)

Summary – Physical and chemical coupling of peatland vegetation, soils and landforms and atmosphere creates feedbacks which may be important in ice-age initiation. A box diffusion CO2 exchange model shows that a transient forcing of 500Gt C (the amount proposed to have accumulated in peatlands during the last interglacial-glacial transition) over 5000 yr results in a lowering of atmospheric CO2 by about 40 ppm. Proxy data indicate that a decrease in atmospheric CO2 may have occurred over the last 5000 years up to pre-industrial times, and the amount (~22 ppm lowering in 5000 yrs) is similar to that calculated from Holocene peatland expansion. These results suggest that models should consider the role of peatlands in ice-age initiation.

View the entire paper here.

In Fig. 2 (see below) we present evidence that prior to the industrial era atmospheric CO2 was undergoing a decline. We attribute the decline to large-scale landscape transformation involving the replacement of forests by peatlands. Peatlands store immense amounts of carbon and, as described in an earlier publication, are potentially powerful organs that help cool the planet.

Peatland formation and ice ages: a possible Gaian mechanism related to vegetation succession

To prepare readers for some upcoming posts on the implications of Gaia theory in climate change predictions I would like to provide some background literature of my earlier work in this area. Below is a paper I gave at the American Geophysical Union Chapman Conference on the Gaia Hypothesis held in San Diego, CA in 1988. This paper was published as a chapter in a 1991 book on the proceedings of the conference: Scientists on Gaia. Here is the summary of my paper:

Peatland formation and ice ages: a possible Gaian mechanism related to vegetation succession

by Lee F. Klinger

Summary – Terrestrial areas, which support over 99% of the earth’s biomass, have considerable potential for being involved in biosphere-atmosphere feedback loops as postulated by the Gaia hypothesis. This paper presents a model of a possible Gaian mechanism related to landscape-level successional changes during a glacial-interglacial cycle. The model is based on the view that terrestrial successions converge toward bogs, rather than toward old-growth forest, and that bogs represent structurally and compositionally stable (climax) communities. The model also assumes, as in classical successional theory, that during the course of succession the biota modifies the environment, both the soil and the atmosphere, to favor the progression of succession toward the climax state. Feedback mechanisms between peatlands (landscapes of bogs and bog forests) and the atmosphere are proposed which should favor the initiation and maintenance of relatively stable, ice age climates. These cooling mechanisms are related to increased albedo, increased evapotranspiration, and decreased atmospheric CO2 associated with the succession from woodlands to peatlands. Ice core and ocean core data for CO2, CH4, and delta 13C and delta 14C isotope ratios are consistent with the proposed terrestrial dynamics involving organic carbon.

Here is the full reference for my paper:

Klinger, L.F. 1991. Peatland formation and ice ages: a possible Gaian mechanism related to vegetation succession (Chap. 28). In: S.H. Schneider & P.J. Boston (eds.), Scientists on Gaia. The MIT Press, Cambridge, pp. 247-255.