We sampled three glacier forelands to assess how ecosystem N retention is affected by succession, and to determine the plant and microbial controls on N retention. (1/x)
As glaciers melt, they expose barren parent material on which succession starts. Because we know exactly when the front of the glacier was where, we know the age of the ecosystems in front of the glacier. This is a great system to test fundamental ecological questions! (2/x)
But in short: we expected N retention to increase with ecosystem age, because soil organic matter builds up, N becomes more limiting, and microbial communities become more fungal-dominated. (4/x)
But this is not what we found! There wasn't a clear pattern with succession, probably because of the huge spatial variation in these systems.
It's clear though that roots and microbes took up most N. (5/x)
But, we did find that plant and microbial properties controlled N retention. Specifically, fast-growing plants and microbes, with low C/N ratio and thus high N demand, took up most nitrogen. In addition, these pools took up more N when soil N availability was low. (6/x)
These findings confirm -in the real world- our earlier findings from a pot experiment that plants and microbes with high N demand take up most N. (7/x) nph.onlinelibrary.wiley.com/doi/10.1111/np…
BUT!!!! They also imply that low N losses in fungal-dominated soils -which is frequently observed- are a consequence of low soil N availability, and not of an inherent high N immobilisation by fungi, which I have suggested in earlier work. (8/x) journals.plos.org/plosone/articl…
OK, so this was only short-term N retention. I'd love to know how this relates to longer-term N retention, and also how different ecosystems in The Netherlands are able to retain N from atmospheric deposition, and how this is affected by other disturbances. (9/x)
So, I thought this was my opus magnum on nitrogen retention, but I might be back for more! (10/end)
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In this study, we show that it's not a good idea to wash roots and immediately collect #root exudates: because of the washing-induced root damage, roots are losing a lot of C and exudate profiles are likely not accurate. (1/6)
Letting the roots recover for a few days before collecting exudates gets rid of this artefact, and allows distinguishing between species and re-application of exudates for mechanistic experiments. (2/6)
Using this 'hybrid' root exudate collection method we were able to show that root traits explain root exudate quantity and quality. (3/6)
De capaciteit om toegevoegd #stikstof vast te houden is een belangrijke functie van ecosystemen: het zorgt voor minder verliezen door uitspoeling en denitrificatie.
Ik wilde specifiek weten of oude ecosystemen meer stikstof kunnen vasthouden dan jonge - dit zou dan komen door meer bodemorganische stof en schimmel-gedomineerde microbiële gemeenschappen in oude ecosystemen. (2/x)
Daarvoor gebruikte ik drie gletsjervoorvelden. Als een gletsjer smelt komt kale rots tevoorschijn, waarop vervolgens bodemvorming en plantengroei begint. Omdat we precies weten wanneer deze gletsjers waar waren, kennen we de leeftijd van de ecosysteempjes in het voorveld. (3/x)
1. Ja, ecosystemen stapelen stikstof, maar de getallen die Staf noemt zijn ongeloofwaardig hoog. In het stuk vergelijk ik deze cijfers met die uit tientallen onderzoeken. (2/x)
2. Ja, ecosystemen maken stikstof vrij uit de bodem, maar het grootste deel van deze stikstof wordt meteen weer opgenomen. Natuurlijke ecosystemen zijn over het algemeen geen “bron” van stikstof. (3/x)
I walked a total of 15k today in my various Zoom meetings, in-person meetings, and phone calls! Pretty grey and chilly though.
I can't recommend this enough. It's so easy: install Zoom on your phone, get a headset that is good for walking, and go! It's a real game-changer for my #mentalhealth and physical health.
I start with my video on, just to day hi, then turn it off and put my phone in my pocket. I also got a battery pack in case my phone battery runs out.