A-Level Biology: Is there much life in a river in late February / early March?
If you stand on a bridge in late February and declare, “This river is dead,” the river will respond by doing what rivers do best: quietly getting on with it while you look at the surface like it’s the whole story.
The big difference at this time of year isn’t whether there’s life, but where it’s hiding and how active it can be, which comes down to temperature, flow, light, and habitat.
1) What “late winter” does to river life (in general)
Late Feb/early March in the UK is usually:
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Cold water → slower enzyme activity, slower metabolism, less visible animal movement.
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Low light / low primary productivity → less algae and plant growth, so less grazing happening in plain sight.
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Higher flows after rain (often) → animals shelter in margins, under stones, in weed beds, and in slower back-eddies.
So: fewer “wow” moments at the surface, but plenty happening below it.
2) Chalk stream River Gade: life with the thermostat left on
Chalk streams are groundwater-fed, so they tend to have clear water, stable flows, and relatively stable temperatures (often quoted around ~10 °C for groundwater-fed systems). That stability gives them longer growing seasons and supports lots of specialist invertebrates.
In late winter on a chalk stream like the Gade, you’re often more likely to find:
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Active macroinvertebrate larvae/nymphs (mayflies, caddisflies, stoneflies—“riverflies”) tucked into gravel, weed, and margins.
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Fish still feeding (not frantic, but not completely “switched off”), helped by that steadier temperature.
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Clearer signs of habitat structure (gravels, ranunculus beds later in spring, undercut banks), which matters because habitat complexity = niches.
In other words: the Gade can look “quiet”, but it’s often quietly busy.
3) River Thames at Bourne End: bigger river, bigger hide-and-seek
The Thames at Bourne End is a larger, slower-to-warm (and often more turbid) lowland river reach. In late winter, you can still have huge biomass present, but it’s typically:
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Deeper and dispersed (fish shoals holding in steadier water)
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More influenced by flow events (spates can shift fine sediment and nudge invertebrates into refuges)
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Less visibly “chalk-stream sparkly” because suspended particles reduce light penetration (so you see less plant/algal action until spring picks up)
But don’t confuse “less visible” with “less alive”: Thames catchment monitoring routinely records diverse macroinvertebrate and plant communities across the system, and seasonal sampling shows that invertebrate communities are there year-round.
4) So… which has “more life” in late Feb/early March?
If you mean most visible life on a quick look:
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Chalk stream (Gade) often wins: clearer water + stable temperature = more obvious signs (and easier sampling success).
If you mean total biomass and variety of habitats:
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Thames can be immense, but you need to sample smartly (margins, slack water, submerged structure) to “see” it.
A nice A-Level way to phrase it:
In late winter, chalk streams often show higher apparent activity and detectability, while large lowland rivers may have equal or greater biomass that is less detectable without targeted sampling.
5) A-Level fieldwork angle: how to test it (properly)
If you want students to compare Gade vs Thames in late winter, make it a mini investigation:
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Standardised kick sample (same time, same net mesh, same number of kicks)
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Record flow, temperature, dissolved oxygen, turbidity, substrate type, channel width/depth
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Identify macroinvertebrates to family level and calculate a biodiversity index (e.g., Simpson’s)
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Optional: focus on EPT groups (mayfly/stonefly/caddis) as a rough indicator set.
You’ll usually find the chalk stream produces “nicer” samples for beginners (cleaner, easier to sort), while the Thames rewards patience and better site choice.
6) A seasonal footnote: “Where are the fish?”
A lot of coarse fish spawning is typically spring/summer as temperatures rise, so late Feb/early March is often more about overwintering behaviour than spawning frenzy.

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