‘One physical system’: Tansley's ecosystem as Earth's critical zone
Summary Integrative concepts of the biosphere, ecosystem, biogeocenosis and, recently, Earth's critical zone embrace scientific disciplines that link matter, energy and organisms in a systems‐level understanding of our remarkable planet. Here, we assert the congruence of Tansley's (1935) v...
| Published in: | New Phytologist |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
2015
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1111/nph.13338 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fnph.13338 https://onlinelibrary.wiley.com/doi/pdf/10.1111/nph.13338 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/nph.13338 https://nph.onlinelibrary.wiley.com/doi/pdf/10.1111/nph.13338 |
| Summary: | Summary Integrative concepts of the biosphere, ecosystem, biogeocenosis and, recently, Earth's critical zone embrace scientific disciplines that link matter, energy and organisms in a systems‐level understanding of our remarkable planet. Here, we assert the congruence of Tansley's (1935) venerable ecosystem concept of ‘one physical system’ with Earth science's critical zone. Ecosystems and critical zones are congruent across spatial–temporal scales from vegetation‐clad weathering profiles and hillslopes, small catchments, landscapes, river basins, continents, to Earth's whole terrestrial surface. What may be less obvious is congruence in the vertical dimension. We use ecosystem metabolism to argue that full accounting of photosynthetically fixed carbon includes respiratory CO 2 and carbonic acid that propagate to the base of the critical zone itself. Although a small fraction of respiration, the downward diffusion of CO 2 helps determine rates of soil formation and, ultimately, ecosystem evolution and resilience. Because life in the upper portions of terrestrial ecosystems significantly affects biogeochemistry throughout weathering profiles, the lower boundaries of most terrestrial ecosystems have been demarcated at depths too shallow to permit a complete understanding of ecosystem structure and function. Opportunities abound to explore connections between upper and lower components of critical‐zone ecosystems, between soils and streams in watersheds, and between plant‐derived CO 2 and deep microbial communities and mineral weathering. Contents Summary 900 I. Introduction 900 II. Tansley's ecosystem as ‘one physical system’ 901 III. Earth's critical zone 901 IV. Historic developments in ecosystem science 902 V. The metabolism of ecosystems and critical zones 905 VI. Towards a more active biogeoscience 908 Acknowledgements 909 References 909 |
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