Phosphorus decline and rescue across soil ages

As soils age primary-mineral phosphorus is depleted and occluded, shifting ecosystems from nitrogen to phosphorus limitation unless plants and microbes mobilise organic and bound phosphorus.

Boundary: where this process starts

Starts with: Primary-mineral phosphorus is depleted by weathering over time

Boundary: where it ends

Ends after: Plants and microbes mobilise P with phosphatases and cluster roots

PARTICIPANTSRESOURCESPlantsMycorrhizalfungiMicrobesMineralsClimatePhosphorusWaterOrganic acidsImpact +3 of 5. Click for details and evidence.Impact -3 of 5. Click for details and evidence.Impact +3 of 5. Click for details and evidence.Impact +3 of 5. Click for details and evidence.Impact +3 of 5. Click for details and evidence.↻ balances · moderate · 0.3 phosphatase relePrimary-mineral phosphorus is depleted by weathering over time: uses up Phosphorususes upPrimary-mineral phosphorus is depleted by weathering over time: uses WaterOccluded and organic phosphorus dominate old soils: uses PhosphorusPlants and microbes mobilise P with phosphatases and cluster roots: makes PhosphorusmakesPlants and microbes mobilise P with phosphatases and cluster roots: uses Organic acidslost from primarymineralsPhosphorus: lost from primary mineralsdrives weatheringreleaseWater: drives weathering releaselocked in occluded formsPhosphorus: locked in occluded formsreleased from organicstoresPhosphorus: released from organic storesdissolvephosphate-beari…Organic acids: dissolve phosphate-bearing mineralsStart: Phosphorusdecline and rescueacross soil agesSTARTStart: Phosphorus decline and rescue across soil agesEnd: Phosphorus declineand rescue across soilagesENDEnd: Phosphorus decline and rescue across soil agesPrimary-mineralphosphorus is depletedby weathering over time📄1 ↗1Primary-mineral phosphorus is depleted by weathering over timeOccluded and organicphosphorus dominate oldsoils📄1Occluded and organic phosphorus dominate old soilsPlants and microbesmobilise P withphosphatases a…📄1 ↗1Plants and microbes mobilise P with phosphatases and cluster roots
Line thickness = size of impact (1 to 5)% on a line = chance a fork takes that branch📄 = pieces of evidence on a stepNegative effectLoops backHypothesisResource used up (arrow into the step)Resource used, not used upResource made or released (arrow out of the step)
What am I looking at? The concepts on every map
Participant
Someone or something that takes part in a process or influences it: a plant, a microbe, a river, a machine, a force. Participants are the rows of a map.
Resource
Something a step uses or uses up: water, oxygen, sunlight, a tool. Each step has an arrow down to the resources it uses.
Step
One thing that happens in a process. Every step has at least one participant and carries evidence.
Decision fork
A step where the process can go several ways. Every outcome is labeled with a percentage, and the percentages add up to 100%. It is not limited to yes or no.
Loop
A line that carries the process back to an earlier step. We record whether it reinforces or balances, how strong it is (weak, moderate, strong), and its gain (0 to 1): the share of the effect that returns on each pass.
Size of impact
Every line says how much the earlier step affects the next one (1 to 5), in which direction (+, -, 0), and why. Thicker lines mean bigger impact.
Evidence
The support for a claim: a source and what it shows. Every step, line, change and vote needs it. Click any step or line to read its evidence.
Boundary
Where a process starts and where it ends. Every process, and every subprocess, has a start and an end.
Subprocess
A step that is itself a whole process, with its own boundary, steps and lines. Click a step marked ↘ to open it. Subprocesses nest as deep as the evidence goes.
Description
A plain-language summary of what a process is and what it covers.
Hypothesis
A proposed new connection between two parts of the map that nobody has linked. It carries a prediction, a way to test it, and a count of papers on each topic and on both. It is an unverified idea until someone tests it.

Every step, with its evidence

The same information as the map, as a list you can search and share. Click a participant or resource to see everywhere it appears.

Primary-mineral phosphorus is depleted by weathering over time
Evidence (1) · added by Broad
  • Walker & Syers 1976, The fate of phosphorus during pedogenesis, Geoderma, doi:10.1016/0016-7061(76)90066-5: Apatite P is lost or transformed during pedogenesis. (confidence 0.8)
Occluded and organic phosphorus dominate old soils
Evidence (1) · added by Broad
  • Peltzer 2010, Understanding ecosystem retrogression, Ecological Monographs, doi:10.1890/09-1552: Ecosystem retrogression: old soils are P-depleted and productivity declines. (confidence 0.7)
Plants and microbes mobilise P with phosphatases and cluster roots
Evidence (1) · added by Broad
  • Lambers 2008, Plant nutrient-acquisition strategies change with soil age, Trends in Ecology & Evolution, doi:10.1016/j.tree.2007.10.008: Plant nutrient-acquisition strategies shift with soil age toward specialised P mobilisation. (confidence 0.75)