EXTINCT ATLAS WIKIEXTINCT LIFE ARCHIVE
Nilssonia (Nilssonia orientalis) · scientific reconstructionView original image

This is an original generative reconstruction, not a photograph or scientific plate.

Nilssonia

Nilssonia orientalis

Long leaves divided into broad segments formed part of the cycadophyte layer beneath Jurassic trees.

Structured expansion · editorial review pending

Time range
About 201–145 million years ago
Final stage
End of the Jurassic
Geographic range
Temperate woodlands of East Asia

What was Nilssonia?

This archive records Nilssonia under the scientific name Nilssonia orientalis, with an age of About 201–145 million years ago and a range of Temperate woodlands of East Asia. Long leaves divided into broad segments formed part of the cycadophyte layer beneath Jurassic trees.

Nilssonia was an extinct cycadophyte whose broad leaf segments attached directly to a central rachis. It shared East Asian forests with ginkgos, conifers and ferns.

Nilssonia at a glance

Scientific name
Nilssonia orientalis
Age
About 201–145 million years ago
Last recorded stage
End of the Jurassic
Known range
Temperate woodlands of East Asia
Broad group
plant
Archive era
Mesozoic
Habitat signals
Forest
Documented regions
Asia

How was Nilssonia built?

Overall body plan

Long leaves divided into broad segments formed part of the cycadophyte layer beneath Jurassic trees.

Growth architecture

The available record is interpreted through preserved proportions, attachment surfaces, wear and comparison with related organisms. For Nilssonia, those observations must be separated from features added only for visual reconstruction.

Reproductive structures

Nilssonia was an extinct cycadophyte whose broad leaf segments attached directly to a central rachis. It shared East Asian forests with ginkgos, conifers and ferns.

Growth and individual variation

A single specimen does not define the whole species. Size, maturity, preservation and possible sex differences are considered before anatomical traits are treated as typical of Nilssonia.

EukaryotaArchaeplastidaPlantaeNilssonia orientalis

How did Nilssonia live?

Nilssonia was an extinct cycadophyte whose broad leaf segments attached directly to a central rachis. It shared East Asian forests with ginkgos, conifers and ferns. This ecological reconstruction is strongest where anatomy, associated organisms and the depositional setting point in the same direction.

What shaped its ecological limits?

Its populations depended on plant communities, soils, water availability and climate. Changes in any one factor did not necessarily cause immediate extinction, but interacting pressures could reduce range, recruitment and resilience.

Where and when did Nilssonia live?

This archive currently lists About 201–145 million years ago; Temperate woodlands of East Asia. Fossil or historical occurrence data describe where evidence has been found, not every place the taxon once occupied. Species-level age and range limits still require source-specific review.

01

Documented geographic range

Temperate woodlands of East Asia. This boundary can change when specimens are reidentified or new localities are published.

02

Time window

About 201–145 million years ago, with the final recorded stage listed as End of the Jurassic. Rock units and dating uncertainty mean the true biological range may extend beyond the known record.

03

Environmental setting

The archive uses the broad habitat labels Forest. These labels help explore related records; a habitat reconstruction requires evidence from individual localities.

What evidence supports reconstructions of Nilssonia?

01

Primary record

Abundant compressed leaves preserve cuticles and stomata; reproductive organs are interpreted through close relatives.

02

Comparative anatomy

Preserved structures are compared with close and functionally similar organisms. The method can constrain posture and function, but analogy alone cannot prove colour, behaviour or soft tissue.

03

Age and locality

Stratigraphy and occurrence records place Nilssonia within About 201–145 million years ago and Temperate woodlands of East Asia. Reworked fossils and uncertain provenance are treated cautiously.

04

Open entity records

Links below connect the archive to available taxonomic and occurrence records. A matching name does not verify every ecological claim, and related-taxon links provide comparison rather than an exact species match.

Why did Nilssonia disappear?

Jurassic and Cretaceous floral turnover reduced many older cycad leaf types before angiosperms expanded.

The last fossil or observation marks the youngest evidence currently known, not necessarily the death of the final individual. Explanations are strongest when timing, environmental change and population biology agree; otherwise the profile preserves uncertainty instead of assigning a single dramatic cause.

Nilssonia FAQ

What was Nilssonia?

This archive records Nilssonia under the scientific name Nilssonia orientalis, with an age of About 201–145 million years ago. Long leaves divided into broad segments formed part of the cycadophyte layer beneath Jurassic trees.

When did Nilssonia live?

The current archive range is About 201–145 million years ago; its youngest recorded stage is End of the Jurassic.

Where was Nilssonia found?

The archive currently lists Temperate woodlands of East Asia. Species-level locality assignments and the full geographic range still require source-specific review.

How do scientists know about Nilssonia?

Abundant compressed leaves preserve cuticles and stomata; reproductive organs are interpreted through close relatives.

Check the source record

Use the scientific name to compare taxonomy, occurrence records and the fossil record. Database coverage and classifications may differ.

How has this record changed?

  1. Completed an AI-assisted bilingual audit of the archive record, corrected identified issues and clarified evidence limits; independent editorial review is pending.
  2. Expanded into a structured bilingual profile with anatomy, ecology, range, evidence, debate and FAQs; independent editorial review is pending.
  3. Verified authoritative entity sources and added three responsive reconstruction sizes.
  4. Initial bilingual species record published.

Found an error or a better source?

Submit a correction