Fossils for Sale - High-quality BRITISH and WORLDWIDE Fossils. An impressive selection of fossils, including Ammonites, Trilobites, Belemnites, Fossil Fish, Fossil Shark Teeth, Fossilised Insects in Amber, Dinosaurs, and Reptiles. UK Fossils was formed in 1988 and collects and preps our own fossils in the heart of the Jurassic Coast, collecting fossils from Lyme Regis, Charmouth and Somerset. Our passion for fossils is reflected in our carefully curated collection, which includes some of the rarest and most unique specimens available.

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Baltic Amber Fossil Barklouse Psocoptera Spread Wings Eocene Insect Inclusion Genuine Fossil with Certificate of Authenticity

£120.00

Genuine Baltic Amber Fossil – Psocoptera Barklouse with Spread Wings

This exceptional Baltic amber specimen contains a beautifully preserved barklouse belonging to the order Psocoptera, captured within ancient tree resin during the Eocene epoch approximately 56–33.9 million years ago. Preserved with wings spread, this delicate insect provides a rare and detailed glimpse into the tiny arthropods that inhabited prehistoric forest ecosystems surrounding the Baltic Sea.

The barklouse became trapped in sticky resin produced by ancient conifer trees millions of years ago. Once enclosed, the resin sealed the insect away from oxygen and microbial decay, preserving the organism in remarkable three-dimensional detail as the resin hardened and fossilised into amber. The fossil displayed in the photographs is the exact specimen you will receive. Each piece is carefully selected to highlight the preserved inclusion. This fossil is a genuine specimen and includes a Certificate of Authenticity lifetime guarantee card.

Geological Origin of Baltic Amber

Baltic amber formed in vast resin-producing forests that flourished across northern Europe during the Eocene epoch of the Paleogene Period. At this time the region experienced warm temperate to subtropical climatic conditions that supported dense forests rich in biodiversity.

The resin responsible for Baltic amber is believed to have been produced by extinct relatives of pine trees often referred to as Pinus succinifera. When these trees experienced environmental stress, storm damage, or insect activity, they exuded viscous resin that flowed down their trunks and branches.

Small organisms moving across bark or vegetation frequently became trapped in the resin. Once sealed within the sticky material, they were protected from decomposition. Over tens of millions of years the resin underwent polymerisation and fossilised into amber.

Many pieces of Baltic amber were transported by ancient rivers and deposited within marine sediments around the Baltic Sea basin. Amber-bearing deposits within glauconitic sands have yielded one of the richest fossil insect assemblages known in the world.

Scientific Classification of the Barklouse

The insect preserved in this specimen belongs to the order Psocoptera, commonly known as barklice or booklice.

Scientific classification

Class: Insecta

Order: Psocoptera

Psocoptera are small insects that typically inhabit tree bark, leaf litter, and forest vegetation where they feed on algae, fungi, lichens, and organic debris. Their presence in ancient forest ecosystems reflects the abundance of microhabitats within tree bark and decaying plant material.

Both winged and wingless species exist, with winged forms often possessing delicate membranous wings held roof-like over the body. In this fossil specimen the wings are preserved in a spread position, allowing the fine wing venation and body structure to be visible.

Morphology and Distinctive Characteristics

Barklice are generally small, soft-bodied insects with relatively large heads, long antennae, and slender legs. Their wings are thin and transparent with characteristic venation patterns that can sometimes be clearly seen in amber fossils.

The insect in this specimen is preserved with wings spread, which is particularly attractive from a visual and scientific perspective. This orientation often reveals the structure of the forewings and hindwings as well as the proportions of the body.

Psocoptera possess chewing mouthparts adapted for feeding on microorganisms and organic material growing on plant surfaces. Their ecological role within forest environments includes recycling organic material and controlling fungal growth on bark and leaves.

Amber preservation frequently retains delicate anatomical details such as wing membranes, antennae, and leg segments. Because amber preserves organisms in three dimensions, the insect may appear remarkably lifelike despite being tens of millions of years old.

Eocene Baltic Forest Environment

During the Eocene epoch the Baltic region supported extensive forests dominated by resin-producing conifers along with a rich diversity of flowering plants. These forests were home to a vast array of insects, spiders, and other arthropods.

Barklice would have lived primarily on tree bark and foliage where they fed on microscopic fungi, lichens, and organic particles. Their small size and slow movements made them particularly susceptible to being trapped by resin flowing down tree trunks.

The sticky resin occasionally captured insects moving across bark surfaces, sealing them inside and preserving them as amber inclusions. Such fossils provide valuable evidence of the microfauna that inhabited these ancient forests.

Amber inclusions like this specimen offer a direct window into prehistoric ecosystems and allow scientists to study organisms that rarely fossilise in other environments.

Amber Preservation and Scientific Importance

Amber is one of the most extraordinary fossil preservation mediums known. Unlike sedimentary fossils that compress organisms into flat impressions, amber preserves organisms in full three-dimensional form.

Baltic amber is especially famous for preserving delicate insects that would otherwise rarely survive in the fossil record. Thousands of insect species have been identified from Baltic amber deposits, providing crucial insights into the biodiversity of Eocene ecosystems.

Psocoptera fossils preserved in amber are particularly important because they document the early evolutionary history of these bark-dwelling insects and the ecological niches they occupied within ancient forests.

Authenticity and Specimen Details

This specimen is a genuine Baltic amber fossil dating to the Eocene epoch approximately 56–33.9 million years ago. The amber has been carefully prepared to reveal the preserved barklouse inclusion while maintaining the natural character of the fossil resin.

The photographs show the exact specimen you will receive. Please refer to the images for full sizing and scale.

Each fossil includes a Certificate of Authenticity lifetime guarantee card confirming that the amber and its inclusion are genuine. This specimen makes an excellent addition to fossil collections, natural history displays, educational collections, or for anyone fascinated by the extraordinary preservation of prehistoric insects within Baltic amber.

(Actual as seen)

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Description

Genuine Baltic Amber Fossil – Psocoptera Barklouse with Spread Wings

This exceptional Baltic amber specimen contains a beautifully preserved barklouse belonging to the order Psocoptera, captured within ancient tree resin during the Eocene epoch approximately 56–33.9 million years ago. Preserved with wings spread, this delicate insect provides a rare and detailed glimpse into the tiny arthropods that inhabited prehistoric forest ecosystems surrounding the Baltic Sea.

The barklouse became trapped in sticky resin produced by ancient conifer trees millions of years ago. Once enclosed, the resin sealed the insect away from oxygen and microbial decay, preserving the organism in remarkable three-dimensional detail as the resin hardened and fossilised into amber. The fossil displayed in the photographs is the exact specimen you will receive. Each piece is carefully selected to highlight the preserved inclusion. This fossil is a genuine specimen and includes a Certificate of Authenticity lifetime guarantee card.

Geological Origin of Baltic Amber

Baltic amber formed in vast resin-producing forests that flourished across northern Europe during the Eocene epoch of the Paleogene Period. At this time the region experienced warm temperate to subtropical climatic conditions that supported dense forests rich in biodiversity.

The resin responsible for Baltic amber is believed to have been produced by extinct relatives of pine trees often referred to as Pinus succinifera. When these trees experienced environmental stress, storm damage, or insect activity, they exuded viscous resin that flowed down their trunks and branches.

Small organisms moving across bark or vegetation frequently became trapped in the resin. Once sealed within the sticky material, they were protected from decomposition. Over tens of millions of years the resin underwent polymerisation and fossilised into amber.

Many pieces of Baltic amber were transported by ancient rivers and deposited within marine sediments around the Baltic Sea basin. Amber-bearing deposits within glauconitic sands have yielded one of the richest fossil insect assemblages known in the world.

Scientific Classification of the Barklouse

The insect preserved in this specimen belongs to the order Psocoptera, commonly known as barklice or booklice.

Scientific classification

Class: Insecta

Order: Psocoptera

Psocoptera are small insects that typically inhabit tree bark, leaf litter, and forest vegetation where they feed on algae, fungi, lichens, and organic debris. Their presence in ancient forest ecosystems reflects the abundance of microhabitats within tree bark and decaying plant material.

Both winged and wingless species exist, with winged forms often possessing delicate membranous wings held roof-like over the body. In this fossil specimen the wings are preserved in a spread position, allowing the fine wing venation and body structure to be visible.

Morphology and Distinctive Characteristics

Barklice are generally small, soft-bodied insects with relatively large heads, long antennae, and slender legs. Their wings are thin and transparent with characteristic venation patterns that can sometimes be clearly seen in amber fossils.

The insect in this specimen is preserved with wings spread, which is particularly attractive from a visual and scientific perspective. This orientation often reveals the structure of the forewings and hindwings as well as the proportions of the body.

Psocoptera possess chewing mouthparts adapted for feeding on microorganisms and organic material growing on plant surfaces. Their ecological role within forest environments includes recycling organic material and controlling fungal growth on bark and leaves.

Amber preservation frequently retains delicate anatomical details such as wing membranes, antennae, and leg segments. Because amber preserves organisms in three dimensions, the insect may appear remarkably lifelike despite being tens of millions of years old.

Eocene Baltic Forest Environment

During the Eocene epoch the Baltic region supported extensive forests dominated by resin-producing conifers along with a rich diversity of flowering plants. These forests were home to a vast array of insects, spiders, and other arthropods.

Barklice would have lived primarily on tree bark and foliage where they fed on microscopic fungi, lichens, and organic particles. Their small size and slow movements made them particularly susceptible to being trapped by resin flowing down tree trunks.

The sticky resin occasionally captured insects moving across bark surfaces, sealing them inside and preserving them as amber inclusions. Such fossils provide valuable evidence of the microfauna that inhabited these ancient forests.

Amber inclusions like this specimen offer a direct window into prehistoric ecosystems and allow scientists to study organisms that rarely fossilise in other environments.

Amber Preservation and Scientific Importance

Amber is one of the most extraordinary fossil preservation mediums known. Unlike sedimentary fossils that compress organisms into flat impressions, amber preserves organisms in full three-dimensional form.

Baltic amber is especially famous for preserving delicate insects that would otherwise rarely survive in the fossil record. Thousands of insect species have been identified from Baltic amber deposits, providing crucial insights into the biodiversity of Eocene ecosystems.

Psocoptera fossils preserved in amber are particularly important because they document the early evolutionary history of these bark-dwelling insects and the ecological niches they occupied within ancient forests.

Authenticity and Specimen Details

This specimen is a genuine Baltic amber fossil dating to the Eocene epoch approximately 56–33.9 million years ago. The amber has been carefully prepared to reveal the preserved barklouse inclusion while maintaining the natural character of the fossil resin.

The photographs show the exact specimen you will receive. Please refer to the images for full sizing and scale.

Each fossil includes a Certificate of Authenticity lifetime guarantee card confirming that the amber and its inclusion are genuine. This specimen makes an excellent addition to fossil collections, natural history displays, educational collections, or for anyone fascinated by the extraordinary preservation of prehistoric insects within Baltic amber.

Additional information

Era

Eocene

Origin

Baltic Sea

Eocene Information

The Eocene Period (56–33.9 million years ago) was a time of warm global temperatures and the rapid evolution of mammals following the extinction of the dinosaurs. The climate was hot and humid, with lush rainforests covering much of the planet, even near the poles. Mammals diversified into new ecological roles, with early primates, whales (like Basilosaurus), large herbivores, and carnivores emerging. Birds and reptiles also thrived, and the first grasses began spreading, setting the stage for later grassland ecosystems. By the late Eocene, the Earth’s climate cooled significantly, leading to the formation of the first Antarctic ice sheets and the eventual transition to the drier, cooler Oligocene Period.

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