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The Birds from Las Hoyas

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Information on the first steps of the avian evolutionary history has dramatically increased during the last few years. The fossil record provides a general view of the morphological changes of the avian flight apparatus from nonvolant ancestors (non-avian theropod dinosaurs) to the first derived fliers of the Early Cretaceous. The Las Hoyas bird record includes three genera: Iberomesornis, Concornis and Eoalulavis. This fossil material has yielded information about the early avian evolutionary history. These Early Cretaceous birds (some 120 Myr old) had a wingbeat cycle and breathing devices similar to those of extant birds. The function of the rectricial fan was also similar. In the evolutionary transition from cursorial ancestors to derived fliers it is possible to verify a trend to increase lift. Primitive wing aspect ratio morphotypes were elliptical ones, other derived morphotypes appeared, for example, in the Neornithes (extant birds). Some primitive fliers, like the Las Hoyas genus Eoalulavis, had an alula (feathers attached to the first digit of the hand) similar to that of present day birds, indicating braking and manoeuvring skills similar to those of their extant relatives. Primitive avian life habits are poorly understood. Some evidence from the Las Hoyas bird record indicates that Early Cretaceous birds were present in the trophic chains.
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Science Progress (2002), 85 (2), 113–130
The birds from Las Hoyas
JOSÉ LUIS SANZ AND FRANCISCO ORTEGA
Information on the first steps of the avian evolutionary history has dramati-
cally increased during the last few years. The fossil record provides a general
view of the morphological changes of the avian flight apparatus from non-
volant ancestors (non-avian theropod dinosaurs) to the first derived fliers
of the Early Cretaceous. The Las Hoyas bird record includes three genera:
Iberomesornis, Concornis and Eoalulavis. This fossil material has yielded
information about the early avian evolutionary history. These Early
Cretaceous birds (some 120 Myr old) had a wingbeat cycle and breathing
devices similar to those of extant birds. The function of the rectricial fan
was also similar. In the evolutionary transition from cursorial ancestors to
derived fliers it is possible to verify a trend to increase lift. Primitive wing
aspect ratio morphotypes were elliptical ones, other derived morphotypes
appeared, for example, in the Neornithes (extant birds). Some primitive
fliers, like the Las Hoyas genus Eoalulavis, had an alula (feathers attached
to the first digit of the hand) similar to that of present day birds, indicating
braking and manoeuvring skills similar to those of their extant relatives.
Primitive avian life habits are poorly understood. Some evidence from the
Las Hoyas bird record indicates that Early Cretaceous birds were present
in the trophic chains.
Keywords: avian evolutionary history
José Luis Sanz is Professor of Paleontology at the Unidad de
Paleontologia. Departamento de Biología, Universidad Autónoma
de Madrid 28049, Cantoblanco, Madrid, Spain. His research fields
are systematics and evolutionary history of several dinosaur
lineages, namely ornithopods, sauropods and birds.
E-mail: jlsanz@inves.es
Francisco Ortega collaborates with the Unidad de Paleontología of
the Universidad Autónoma de Madrid (Spain) in several Las Hoyas
research projects. His research fields are systematics of archosaurs
(crocodilians, dinosaurs and birds, between others).
E-mail: francisco.ortega@uam.es
113
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Introduction
Some 120 million years ago (Early Cretaceous) a shallow lake existed
in the Serranía de Cuenca (East–Central Spain). The sediments of this
paleolake, known as Las Hoyas, consist of rhythmically fine-grained
laminated limestones preserving such delicate structures as dinosaur
muscle tissues, gut contents or feathers
1,2
(Figure 1). The Las Hoyas
limestones have yielded a diverse flora and fauna emerging from
both aquatic and terrestrial biota. The floral assemblage includes
charophytes, bryophytes, filicales, bennettitales, gnetales, coniferales
and angiosperms. Animal remains belong to bivalves, gastropods,
crustaceans, insects, myriapods, bony fishes, albanerpetontids,
anurans, urodelans, turtles, lizards, crocodiles, dinosaurs and birds
3,4
.
The current bird assemblage from Las Hoyas includes three species:
Iberomesornis romerali, Concornis lacustris and Eoalulavis hoyasi.
Our knowledge about the avian evolutionary history has dramati-
cally improved during the last two decades. This increase of infor-
mation about the first steps of bird evolution comes from two sources:
our better knowledge of the Mesozoic fossil record, and the phylo-
genetic systematics (cladistics) approach. Cladistics has allowed
more robust and feasible genealogical hypotheses which are the nec-
essary first step for understanding the evolutionary history of every
lineage. Twenty years ago a gap in the record existed between the
oldest known bird (Archaeopteryx, Upper Jurassic) and the Upper
Cretaceous toothed birds (Hesperornithiformes and Ichthyornithi-
formes). During the last few years significant discoveries have been
made in the Early Cretaceous of Spain (Las Hoyas) and China
(Yixian Formation, Liaoning Province) This new evidences along
with other data from Argentina and Madagascar, have radically
114 José Luis Sanz and Francisco Ortega
Fig. 1. Fluorescence-induced ultraviolet photograph of the
ornithomimosaur theropod dinosaur Pelecanimimus polyodon from the
Las Hoyas lithographic limestones. Arrow indicates a soft tissue crest at
the posterior side of skull.
SP/Ortega 9/7/02 10:06 am Page 114
changed our ideas about early avian history with respect to important
topics as historical diversity, origin and development of flight,
feather origin, or life habits of the primitive birds. Nearly half of the
present day Mesozoic genera have been described after 1990
5
. Thus,
we know that upper Mesozoic avian diversity was much larger than
previously supposed, and the present day birds (Neornithes) are a
particular lineage coming from a Cretaceous bird lineage. On the other
hand, modern avian flight appears during the Early Cretaceous, and
feathers are an evolutionary novelty that appeared in the bird ances-
tors, the non-avian theropod dinosaurs. Early Cretaceous birds were
constant components of the terrestrial ecosystems all around the world.
This paper deals with the information yielded by the Las Hoyas birds
related to some of these aforementioned research topics, especially
concerning the development of the modern flight and life habits of the
primitive birds
The Las Hoyas bird Record
The first avian species found at Las Hoyas was Iberomesornis romerali,
a sparrow-sized small animal (Figure 2) whose mass has been esti-
mated
6
between 15 and 20 g. The specimen is almost complete, lack-
ing the skull and the anterior cervical vertebrae. Iberomesornis is
characterised by a singular combination of traits, including some
primitive ones, present in the non avian theropods, like a sacrum
composed of five vertebrae, tarsal not fused to the tibia or to the
metatarsals, and lacking any evidence of metatarsal fusion. Along with
these symplesiomorfic features, Iberomesornis shares with modern
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Fig. 2. Iberomesornis romerali.
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birds a number of evolutionary novelties: a derived, modern avian
furcula, with a low interclavicular angle, strut-like coracoids, and a
series of free caudal vertebrae (eight in number) and a large pygo-
style composed by the fusion of 10–15 vertebrae
7–9
(Figure 3). This
combination of primitive and derived traits led Sanz et al., 1988 to
propose a phylogenetic hypothesis for this Las Hoyas bird, placing it
in an intermediate position between Archaeopteryx and modern
birds. The introduction within the avian ingroup of the Early
Cretaceous Chinese genus Confuciusornis, along with the reinter-
pretation of some characters, has recently modified this early phylo-
genetic hypothesis for Iberomesornis. The present proposal is that this
primitive Spanish bird is more closely related to the enantiornithine
birds than previously supposed
10,11
(see phylogenetic hypothesis of
Figure 4).
The Enantiornithes are an extinct group of Cretaceous birds
described, for the first time, by Walker in 1981, in the North of
Argentina. We now know that this avian lineage have a world-wide
distribution, whose remains have been discovered in both Americas,
China, Mongolia, Australia and Spain. The Spanish enantiornithine
record comes from Las Hoyas and the Montsec
12
(Province of Lleida).
Two enantiornithine genera have been described in Las Hoyas:
Concornis and Eoalulavis. The first one (type species C. lacustris) is
about twice the size of Iberomesornis, and it is recognised by an almost
complete skeleton lacking the skull and neck with some feathers evi-
dence
6,13
. One of the most singular features of Concornis is the sternal
morphology (Figure 5). The sternum has a carina developed just in its
caudal half, with two crests diverging from its anterior region. The
116 José Luis Sanz and Francisco Ortega
Fig. 3. Iberomesornis romerali. Fluorescence induced ultraviolet photo.
SP/Ortega 9/7/02 10:06 am Page 116
sternal caudal zone is deeply notched, in a configuration similar to
that of the Chinese genus Cathayornis
14
. The furcular morphology is
derived with an interclavicular angle of some 60°. The hand is
slightly shorter than the forearm and the femur clearly shorter than
the tibiotarsus. The fossil remains in which the species Eoalulavis
hoyasi is based consist of the anterior part of an articulated skeleton
lacking the skull and anterior cervical vertebrae (Figure 6). This beauti-
fully preserved specimen includes evidence of wing feathers in position
(both primary and secondary ones) and the alula (feathers attached to
the first digit of the hand). Some body feathers are visible around the
humeri and pectoral girdle. Again, the sternal morphology is charac-
teristic, but very different to that of Concornis. The sternum of
Eoalulavis is lanceolated, with a foot-like caudal expansion, possessing
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Fig. 4. Cladogram showing a hypothesis of the avian phylogenetic
relationships.
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a faint carina. The anterior sternal third has a narrow cleft, in which
the extremely long hypocleidium (posterior process of the furcula)
probable fits
15
. Both Concornis and Eoalulavis present a series of
evolutionary novelties, mainly in the coracoid, humeri and metatarsi,
typical of enantiornithine birds. The internal relationships within this
clade is poorly understood, but most authors agree on its mono-
phyletic status
11,13,16
.
The avian flight
The evolutionary success of birds is probably related to its skills
for flying. From the ancestral groups (cursorial non-avian theropod
118 José Luis Sanz and Francisco Ortega
Fig. 5. The enantiornithine bird from Las Hoyas Concornis lacustris.
SP/Ortega 9/7/02 10:06 am Page 118
dinosaurs), descendants with flying capabilities appeared. The known
avian fossil record yields general information on the historical morpho-
logical changes produced in this process, from non-volant to volant
forms. Most of the evolutionary novelties of this sequence of morpho-
logical changes are related to the avian flight apparatus, composed of
bones, muscles and feathers. The bird fossil record offers information
on bones and feathers, but the phylogenetic functional morphology
presents information about muscles and associated ligaments. Thus,
from the most primitive bird (Archaeopteryx) to modern extant birds
(Neornithes) a series of evolutionary novelties related to the flight
apparatus improved the flight skills of this group of volant theropod
dinosaurs
6,8,17,18
.
The morphological change sequence of the flight apparatus has to
be analysed in terms of physical forces. Flight requires a combination
of lift and thrust. In the avian flight the wings, by means of a set of
upstroke and downstroke movements, provide both forces. Weight
generated by the pull of gravity has to be balanced by the lift pro-
vided by the wings. But lift is not the only aerodynamic effect of the
wings: a drag force is also generated, that has to be balanced by the
propulsion forces (thrust). Besides the wings, other elements of the
avian flight apparatus are significant elements in the volant locomotion.
For example, the appearance of a rectricial fan is very important in
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Fig. 6. Eoalulavis hoyasi. Top, fluorescence induced ultraviolet photo of
the specimen before preparation. Bottom, reconstruction. A: alula; PR:
primary remiges; SR: Secondary remiges.
SP/Ortega 9/7/02 10:06 am Page 119
order to permit steering and braking. On the other hand, a complex
combination of evolutionary novelties is characteristic of the avian
respiratory system (lungs and aerial sacs) which are relevant in the
conquest of the aerial environment. Thus, after obtaining some infor-
mation on the flight skills of Archaeopteryx we will see that the
information provided by the Las Hoyas birds is related to three topics:
wing and tail biomechanics, wing evolutionary history, and function
of the respiratory system.
Wing and tail biomechanics
The skeleton and feather systems of Archaeopteryx are very similar
to those of the most derived non-avian theropods. The retention of a
primitive cursorial locomotor module composed by the decoupling
of tail and hindlimbs
19
, is combined with the presence of some avian
synapomorphies like the relative elongation of the forelimb or the
angle between the scapula and coracoid. However, the glenoid cav-
ity (pectoral girdle humeral articulation region) is oriented in a way
similar to that of non-avian theropods, implying a smaller efficiency
in the wingbeat cycle. The present consensus is that Archaeopteryx
was not merely a glider, but could probably perform some kind of
powered flight, although not as efficiently as extant birds.
Archaeopteryx was probably capable of taking off from the ground,
because of the added thrust provided by its hind limbs
20
. Nevertheless,
its capabilities of performing a low speed flight and its manoeuvr-
ability skills were probably limited.
From the forerunner condition present in Archaeopteryx, a series
of evolutionary novelties appeared in the avian lineage, which
implies more efficiency in the volant locomotion. This synapo-
morphies related with the improved flying skills are present in birds
120 million years old, as the Chinese genus Confuciusornis or the
Las Hoyas genera Iberomesornis, Concornis and Eoalulavis.
Thus, we will see that the functional interpretation of the three
skeletal zones (pectoral girdle, furcula and pygostyle) is modified
regarding the conditions present in a primitive flyer as Archaeopteryx.
The coracoid of Archaeopteryx is short, and subquadrangular in
shape. The derived coracoidal morphology (strut-like) is typical of
modern birds, but is also present in the primitive birds from Las
Hoyas
6,7,8,13,15
. This type of derived coracoid indicates, as in Neornithes,
the existence of a complex biomechanical system (triosseum foramen)
formed by the scapula, furcula and coracoids. This structure pro-
vides the mechanism for the ligament of the supracoracoideus
muscle, working as a pulley-like system during the upstroke phase of
120 José Luis Sanz and Francisco Ortega
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the wingbeat cycle. Recent analysis has concluded that this system
not only abduces the wing, but also produces a horizontal rotation of
the humerus, to position the wings for the downstroke
21
. The presence
of a triosseum foramen in Las Hoyas birds suggest that in these genera,
there is a wingbeat cycle mechanism similar to that of extant birds.
The furcular morphology of Archaeopteryx is primitive, with inter-
clavicular angle near 90°. This primitive morphology is retained by
the basal pygostylian birds, Confuciusornis and Changchengornis
(Confuciusornithidae
22
). Iberomesornis presents a derived avian fur-
cula, with a low interclavicular angle and a developed hypocleidium.
This type of modern furcula is very important in flight performance,
because of the large amount of oxygen needed during the powered
flight. The main function of the furcula is contribute to the ventila-
tion of the lungs and air sacs during the active flight
23
. Thus, it is
very probable that some primitive birds, like the Las Hoyas genera,
had a similar breathing mechanism to that of their extant relatives.
The clade Pygostylia (see Figure 4) is characterised by an evolu-
tionary novelty that dramatically changes the primitive tail morphol-
ogy present in Archaeopteryx. Basal pygostylians, like the
Confuciusornithidae, or more derived, like Iberomesornis, have fused
caudal vertebrae into a single element (pygostyle). In Archaeopteryx,
the relative long feathered tail could have helped to increase the lift,
but the aerodynamic efficiency seems to be low. The presence of a
pygostyle implies the existence of a Parson’s nose, with rectrice
feathers along with a rectricial bulb (that in extant birds facilitates
the opening and closing of the fan of caudal feathers). This structure
is relevant during the flight since allows a greater manoeuvrability,
improves the steering and braking capabilities, and increases the
lift
6,9
(Figure 7).
In summary, the flying skills of some Early Cretaceous birds, such
as Iberomesornis, would be improved with respect to those of
Archaeopteryx. Iberomesornis had better wingbeat cycles and
breathing mechanisms, as well as caudal fan functions. Neverthe-
less, this Las Hoyas bird cannot be considered as a volant form with
flying capabilities equivalent to those of its extant relatives. In pre-
sent day birds, locomotion is characterized by the relationships
between three locomotor modules: pectoral, hind limbs and tail
19
.
There is a decoupling between the hind limb and tail modules (the
tail is no longer involved in cursorial locomotion) and there is a new
allegiance between the pectoral and tail ones for performing flight.
In Iberomesornis, the presence of derived wing proportions, cora-
coid and furcula, correlated with a large pygostyle, suggest that the
allegiance between the pectoral and tail modules began to be formed,
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whereas the decoupling between hind limb and tail modules was not
complete. In conclusion, Iberomesornis flight skills have to be con-
sidered as intermediate between the primitive volant condition rep-
resented by Archaeopteryx and the sophisticated flight capabilities of
the extant birds.
122 José Luis Sanz and Francisco Ortega
Fig. 7. Life reconstruction of a couple of flying Iberomesornis.
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Wing evolutionary history
During the avian flight locomotion, lift depends on several factors:
wing size, air speed, air density, and the angle of attack (angle of the
wing with respect to the trajectory)
24,25
. In the evolutionary transition
from non-avian dinosaurs to birds an improvement of the flight skills
is expected. In fact, the morphological transformations of the skele-
tal flight apparatus allow us to propose a sequence composed of three
stages:
(1) non-avian dinosaurs showing the cursorial condition;
(2) primitive fliers, such as Archaeopteryx, making up an intermedi-
ate stage; and
(3) derived fliers, such as some primitive birds like Confuciusornis,
and basal ornithothoracines like Iberomesornis.
In the evolutionary transition from cursorial ancestors to derived
fliers, one of the locomotory physical requirements is for lift to be
increased. The increase of lift in primitive fliers can be evaluated in
terms of the wing loading. The wing loading (WL) is the estimation
of the lift of a wing by means of the ratio W/S, in which W= weight
and S= wing area, the latter is the surface projected by the fully
extended wings and the portion of body situated between them
26
.
Thus, it is expected that the decrease of the wing loading from mem-
bers of Stage 1, i.e. feathered dinosaurs such as Protarchaeopteryx
or Caudipteryx, to Archaeopteryx, and from the latter to the mem-
bers of Stage 3.
In order to check this hypothesis we need to know or estimate both
the weight and the wing area of taxa involved in the origin and
development of avian flight.
Weight estimation is based on the equation: FL = 0.5659
W
0.3424
, resulting from a regression analysis of femur length (FL) on
weight in 65 species of extant birds representing 13 different
orders
27
. In the same way, wing area is estimated using the equation:
S = 0.052 + 0.008 W, for a regression analysis of weight on wing
area from a 120 extant birds based on ref. 25.
The results support the formulated hypothesis: wing loading
decrease from probable non-flying forms, like Caudipteryx and
Protarchaeopteryx
28
, to primitive fliers, like Archaeopteryx and
from this to the first derived fliers (Confuciusornis and basal
ornithothoracine birds). However, an unexpected increase of the
wing loading began with the clade Ornithurae. If the hypothesis we
propose is correct, then large wing loading values in extant birds are
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a reversal of the derived character states of the primitive condition,
probably related to different types of flight performance. For exam-
ple, cruising speed depends on wing loading. The greater the value
of this ratio, the faster the bird is able to fly
25
.
Another factor determining the flight performance is the shape of
the wing or aspect ratio. This is defined as the ratio between length
(span) and width (chord) of the wing. Based on the aspect ratio, there
are five basic types of wings
24,29
. The elliptical morphotype is
characterised by a slenderness, that is, span dimension is small
relative to chord. This morphotype is characteristic of most Passeri-
formes and doves, which have high manoeuvrability. Long soaring
(gliding) wings are morphotypes with a high aspect ratio, and are pre-
sent in albatrosses and gulls, that is, high-speed soarers
26
. Short soar-
ing wings are morphotypes with intermediate aspect ratios between
long soaring and elliptical morphotypes. They are characteristic of
vultures, storks, and eagles, that is, low-speed soarers. Swallows and
martins have high-speed wings, which are characteristically bowed
and acuminated. Finally, there is the hovering morphotype, which is
typical of hummingbirds. Hovering flight is characterized by the
absence of a thrust component, only a lift component. This type of
flight performance requires a large energy input.
The fossil evidence of wing aspect ratio is scarce. Only excep-
tionally well-preserved specimens, i.e. the Berlin Archaeopteryx,
show its wing aspect ratio. In most fossils, wing aspect ratio is not
preserved and a reconstruction exercise is necessary. In these condi-
tions, it is difficult to propose even a general evolutionary pattern of
wing aspect ratio. Nevertheless, some conclusions can be made. The
elliptical wing morphotype seems to be primitive within Aves. It
shares several conditions such as being present in Archaeopteryx and
probably in basal ornithothoracine birds, and being the least special-
ized and most frequent type of wing. This primitive wing aspect ratio
could be the condition widespread among Enantiornithes. Derived
aspect ratio morphotypes (long and short soaring, high-speed, hov-
ering morphotypes) appeared, at least, in the Neornithes, and proba-
bly within more inclusive clades. As in the case of wing loading,
aspect ratio diversity can be related to different bird life habits asso-
ciated with different flight requirements.
One of the most important features in the evolutionary history of
avian flight is a trend towards reducing drag. When a bird is trying to
reduce speed, it extends the alula generating an additional air flux
that reduces the eddying that occurs at the posterodorsal zone of the
wing, reducing or even eliminating problems of lift maintenance.
The most primitive known fossils showing alula evidence are
124 José Luis Sanz and Francisco Ortega
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the Early Cretaceous enantiornithine birds Eoalulavis
15
and
Eoenantiornis
30
. The alula feathers of Eoalulavis have a derived
asymmetric vane, showing no structural differences with the alula
feathers of extant birds. However, it is probable that in Eoalulavis
alula feathers were fewer in number than in extant birds. No alulas
are known outside the clade ornithothoraces. Both, Archaeopteryx
and the well-known Confuciusornis, lack the alula
22
. Thus, the must
likely hypothesis is that the alula appeared as an evolutionary
novelty in ornithothoraces.
Respiratory system
In order to support the large levels of muscular work involved in
flight, birds need a highly efficient respiratory system. The performance
www.scilet.com The birds from Las Hoyas 125
Fig. 8. Pellet, probably from a theropod dinosaur, containing fossil
remains of, at least, three different species of primitive birds.
SP/Ortega 9/7/02 10:06 am Page 125
of flight at high altitude probably was a problem in the evolutionary
history of birds, as there seems to be a decrease of oxygen pressure
with height. The respiratory system of the extant bird is made of
lungs and air sacs
31, 32
that permit efficient ventilation even in lower
oxygen pressure environments. It seems very probable that aerial
sacs were present in the avian ancestral groups. It is also probable
that some primitive birds like Iberomesornis, with a derived flying
apparatus, had improved the functional levels of their air sacs. But
these primitive birds lacked the pneumatic foramina, present in
extant birds in several bones (vertebrae, humerus, sternum, etc). If
this absence indicates a lesser efficiency of the respiratory system,
then it is possible to formulate a hypothesis about the existence in
bird evolutionary history of a trend to produce forms with increasing
skills to perform flight at lower atmospheric oxygen pressure. If the
oxygen pressure levels of the Mesozoic atmosphere were similar to
those of the present day, birds progressively acquired a better cap-
ability to fly at elevated altitude. Thus, it seems probable that primi-
tive fliers such as Archaeopteryx were able to reach a low ceiling-
height, and a long evolutionary trend occurred until the appearance
of present day high-altitude soarers.
126 José Luis Sanz and Francisco Ortega
Fig. 9. SEM photograph of one of the tiny avian long bones of the pellet
illustrated in Fig. 8.
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Primitive bird life habits
The presence of birds (both in terms of population density and diver-
sity) in the terrestrial Early Cretaceous ecosystems is clearly more
important than previously supposed. Nevertheless, the life habits of
these primitive birds are poorly known. The avian fossil record of
Las Hoyas has provided some information related to the position of
some Early Cretaceous birds in the trophic chains.
The thoracic box of Eoalulavis contains organics particles identi-
fied as exoskeletal elements of unidentified crustaceans: the oldest
known direct evidence of trophic habits for birds
15
. This evidence
seems to support some kind of life habit related to aquatic environ-
ments.
Another avian material found at the Las Hoyas site yielded evi-
dence about the role of birds in the Mesozoic trophic chains. The fossil
is made of a bone assemblage (about 23 cm
2
in surface area) coming
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Fig. 10. Life reconstruction of the probable pellet producer of the fossil
illustrated in Fig. 8.
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from four tiny juvenile bird individuals (Figure 8). Some morpho-
logical differences and size divergences indicate that the fossil bone
assemblage comes from at least three different species. The most
parsimonious hypothesis to interpret this fossil is that an organic
agent was responsible for this bird bone assemblage, resulting from
a predator that produced a regurgitated pellet
33
. This hypothesis is
supported by the SEM observation of the bones: its surface (perios-
teum) shows the characteristic pitting of digested bones of birds and
mammals (Figure 9). But the identification of the predator is prob-
lematic. Based on the actual and putative predator fossil record of
Las Hoyas, the most probable producer of this fossil pellet was a
large pterosaur or a small-medium sized theropod dinosaurs (Figure
10). This fossil pellet clearly indicates that birds were usual prey in
the Early Cretaceous terrestrial ecosystems
Acknowledgements
We thank all the co-authors of our previous publications and co-
workers at the Las Hoyas projects for stimulating the ideas and
research discussed here. We want also thank to M. Anton and
R. Martín for reconstruction of Eoalulavis and Iberomesornis and
G. F. Kurtz for UV photographs. Work in Las Hoyas fossil site has
been supported by funds from Junta de Comunidades de Castilla-La
Mancha, Spanish DGICYT and European Union.
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... Radiometric dating using U-Pb from zircons found in the volcanoclastic matrix surrounding the amber has refined this age, providing an absolute estimate of 98.8 ± 0.6 Ma (Shi et al., 2012). This means that these amber specimens help to fill an important gap between the well-known Early Cretaceous avifaunas from China and Spain that are Barremian to Aptian (Sanz and Ortega, 2002;Pan et al., 2013) and Late Cretaceous specimens from North and South America that range from the Coniacian to Maastrichtian (Chiappe, 1993;Atterholt et al., 2018). ...
... The very small body size and unfused proximal carpometacarpus suggest that YLSNHM00813 is an immature individual. Similar to the immature holotype of Iberomesornis romerali (Sanz and Ortega, 2002), the minor metacarpal does not project farther distally than the major metacarpal as it does in most of the other enantiornithines Frontiers in Earth Science | www.frontiersin.org (Chiappe and Walker, 2002). ...
Article
Full-text available
Recent discoveries of enantiornithine birds trapped in amber have decreased the lower size limit of members of this clade, increased their morphological diversity, and provided significant new data regarding their plumage. Here, we describe a new specimen that consists of the distal extremities of both forelimbs and hindlimbs. Size and morphology suggest the specimen represents an immature individual. Although the skeletal morphology is poorly preserved, the new specimen most probably represents a member of the Enantiornithes based on the sum of its preserved morphologies, including its small size, elongate penultimate pedal phalanges, and large recurved unguals. Based on the lengths of the metatarsals, the new specimen is even smaller than previously described enantiornithines that preserve these elements; however, the forelimb elements are longer than those in the only other specimen preserving comparable overlapping skeletal material. This is suggestive of a diversity of limb proportions in the Burmese enantiornithine fauna, similar to that observed in the Jehol avifauna, in which intermembral indices range from approximately 1 to 1.5. The wing appears to consist of eight primaries, less than that of neornithines, contributing to mounting data that suggests the flight apparatus of enantiornithines was unique from that of other basal birds and neornithines. The well-preserved flight feathers are ornamented with pale basal bands, further adding to the diversity of Cretaceous plumage patterns revealed by Burmese amber specimens.
... Das questões abordadas neste trabalho podemos discutir a ocorrência de uma Enanthiornites no Barremiano do Espichel. Relativamente a esta questão há a referir que estão descritos em Espanha restos de pequenas Enantiornithes, na formação de Las Hoyas (Sanz & Ortega, 2002), também datada do Barremiano. As Enantiornithes foram um grupo de aves mais diversificado do Cretácico, com uma grande diversidade de tamanhos (Walker, et al. 2007). ...
... As Enantiornithes foram um grupo de aves mais diversificado do Cretácico, com uma grande diversidade de tamanhos (Walker, et al. 2007). Os estudos apontam para que os individuos de Areias de Mastro tivesse uma envergadura de asas perto de um metro, o que o diferencia das Enantiornithes de Espanha, que tinham um pequeno porte (Sanz & Ortega, 2002). Devido à escassez de fósseis de aves miocénicas de Portugal, não foi possível fazer um estudo comparativo direto. ...
Article
Full-text available
We present the fossil record of birds in Portugal, with emphasis for the earlier Pleistocene deposits. This work consisted in bibliographical survey about the remains of birds already described and published and in the study of a set of remains of fossil birds not yet published, most of which are on deposit at the geological Museum, in Lisbon. There are few published studies on fossil birds of Portugal, specially birds that existed before the Pleistocene. The few publications about Mesozoic and Cenozoic birds in Portugal was done by Zbyszewski and Ferreira, 1967; Antunes, 1981; Harrison, 1983; Sanches-Marco, 1987, who makes a resume about the Miocene birds of Portugal; Weigert, 1995; Mourer-Chauviré and Antunes, 2003 and Gerald et al., 2008. Of these, only five are specifically about bird fossil remains. The earliest known fossil of birds in Portugal date from the late Jurassic: a tooth that Weigert attributed to Cf. Archaeopteryx. With the exception of an ulna, possibly from a bird, found in the Cabo Espichel, there aren’t any more known remains of Mesozoic birds in Portugal. From Cenozoic are reported, in some publications, seven palaeontological sites: Silveirinha, (Eocene), where Harrison has identified a charadriiforme (Fluviatilavis antunesi), Penedo-Sesimbra, Aveiras de Baixo and Amor – Leiria (Miocene), were mentioned unidentified bird. In Lisbon, two Miocene bird remains were found in Olival da Susana (a Paleoperdix) and, in Quinta das Pedreiras (a gruidae). In Costa da Caparica – Almada, one sternum of Pelagornis miocaenus was discovered in 1976 and described by Gerald et al, in 2008. In the Geological Museum of Lisbon there is a collection of fossils from the Miocene birds not yet published, that are studied in this work. This is a set of 9 remains from 5 Miocene deposits: Quinta das Freiras e Olival da Susana, in Lisboa, Anchino and Barreiro do Oleiro, near Vila Nova da Rainha and Aveiras de Baixo; they belong to three groups of birds: Passeriformes, Anseriformes and Galliformes. From Praia do Penedo more rests of birds were identified, belonging to the Suliformes. The most bird species identified from the Pleistocene are identified species still exist today. Of a total of 80 species identified as dating from the Portuguese Pleistocene, only 8 (10%) are extinct today or no longer live in the wild in Portugal. Some of them still live in other parts of Europe, such as the Pyrrhocorax graculus, the Cygnus olor and the Mergellus albellus; only the Pinguinus impennis and the Corvus antecorax are known to be really extinct.
... Inspection of the matrix (Fig. 1A,C) rules out preparation marks as a possible origin of these structures. Furthermore, the LSF images are consistent with the morphology of the Las Hoyas specimens Eoalulavis MPCM-LH-13500 13,14 , Concornis MPCM-LH-2814 13,15,16 and isolated feathers 4 www.nature.com/scientificreports www.nature.com/scientificreports/ ...
... Inspection of the matrix (Fig. 1A,C) rules out preparation marks as a possible origin of these structures. Furthermore, the LSF images are consistent with the morphology of the Las Hoyas specimens Eoalulavis MPCM-LH-13500 13,14 , Concornis MPCM-LH-2814 13,15,16 and isolated feathers 4 www.nature.com/scientificreports www.nature.com/scientificreports/ ...
Article
Full-text available
Laser-Stimulated Fluorescence (LSF) is used to identify fully fledged feathering in the hatchling enantiornithine bird specimen MPCM-LH-26189, supporting precocial nesting behavior in this extinct group. The LSF results include the detection of a long pennaceous wing feather as well as cover feathers around the body. The LSF technique showed improved detection limits over and above synchrotron and UV imaging which had both been performed on this specimen. The findings underscore the value of using a wide range of analytical techniques.
... On the basis of morphological and size data, at least three different species are present in the fossil bone assemblage. The most possible producer of the pellet was a small-to medium-sized nonavian theropod or a large pterosaur (Sanz et al., 2001b;Sanz and Ortega, 2002). ...
... El yacimiento de Las Hoyas ha proporcionado un relativamente abundante registro de terópodos avianos, de los que, hasta el momento se han descrito tres géneros de enantiornitas: Iberomesornis, Concornis y Eoalulavis (Sanz et al., 1988;Sanz y Bonaparte, 1992;Sanz y Buscalioni, 1992;Sanz y Ortega, 2002; (fig. 3c). ...
Article
Body fossils of the Iberian Peninsula dinosaurs are very relevant for the knowledge of several aspects of the evolutionary history of the group, and, in addition, for the interpretation of the distribution of many of its components, due to the geographic situation of the Iberian Peninsula. Almost all of the groups of dinosaurs are represented in the Iberian Peninsula record: ornithopods, thyreophorans, theropods and sauropods. These groups are present, mainly, in the transit Jurassic-Cretaceous (Kimmeridigian-Berriasian), the upper part of the Lower Cretaceous (Barremian-Aptian) and in the end of the Upper Cretaceous (Campanian-Masstrichtian). Ornithischian dinosaurs are represented by thyreophorans such as the stegosaurians Dacentrurus and Stegosaurus, the ankylosaurs Dracopelta, Polacanthus and Struthiosaurus, and ornithopods like hypsilophodontids, basal iguanodontians (Rhabdodori), dryosaurids, camptosaurids (Draconyx and Camptosaurus), iguanodontids (Iguanodon) and hadrosaurids (Pararnabdodon). Some Incertae sedis and taxa in process of description are present too. Sauropods are represented by taxa related to Neosauropoda (Lourinhasaurus, Dinheirosaurus, Galveosaurus-and Losillasaurus) and titanosauriforms (Aragosaurus, Lusotitan and Lirainosaurus). In addition, new forms are still in description, like the sauropods of Riodeva (Teruel), Penarroya de Tastavins (Teruel) and Morella (Castellón). Theropods are represented by the ceratosaurian Ceratosaurus, the spinosauroid Torvosaurus, the carnosaurs Lourinhanosaurus and Allosaurus, the tyrannosaurid Aviatyrannis, the ornithomimosaur Pelecanimimus, and the avian-theropods Iberomesornis, Concornis, Eoalulavis and Noguerornis. Nevertheless, theropods diversity is more abundant as it shows the great variability of teeth morphotypes identified.
... On the basis of morphological and size data, at least three different species are present in the fossil bone assemblage. The most possible producer of the pellet was a small-to medium-sized nonavian theropod or a large pterosaur (Sanz et al., 2001b;Sanz and Ortega, 2002). ...
... This general conclusion is further reinforced by the relatively short primary feathers we report here. The morphology of fossils, including the presence of aerodynamic control features such as an alula and wingtip feather separation, suggests that some enantiornithine birds possessed more sophisticated flight abilities than Archaeopteryx (Sanz et al., 1996;Garner et al., 1999;Zhang & Zhou, 2000;O'Connor et al., 2009), although still limited when compared to the diversity seen in modern birds (Sanz & Ortega, 2002;Zhou & Zhang, 2007). Surveys of forelimb proportions have also shown that these birds fall within the range of extant taxa and thus likely possessed at least some of the flight styles of their living counterparts ). ...
Article
We examine the relationships between primary feather length (f(prim)) and total arm length (ta) (sum of humerus, ulna and manus lengths) in Mesozoic fossil birds to address one aspect of avian wing shape evolution. Analyses show that there are significant differences in the composition of the wing between the known lineages of basal birds and that mean f(prim) (relative to ta length) is significantly shorter in Archaeopteryx and enantiornithines than it is in Confuciusornithidae and in living birds. Based on outgroup comparisons with nonavian theropods that preserve forelimb primary feathers, we show that the possession of a relatively shorter f(prim) (relative to ta length) must be the primitive condition for Aves. There is also a clear phylogenetic trend in relative primary feather length throughout bird evolution: our analyses demonstrate that the f(prim)/ta ratio increases among successive lineages of Mesozoic birds towards the crown of the tree ('modern birds'; Neornithes). Variance in this ratio also coincides with the enormous evolutionary radiation at the base of Neornithes. Because the f(prim)/ta ratio is linked to flight mode and performance in living birds, further comparisons of wing proportions among Mesozoic avians will prove informative and certainly imply that the aerial locomotion of the Early Cretaceous Confuciusornis was very different to other extinct and living birds.
... Pelecanimimus permitió interpretar que esta condición puede tener como estado previo el desarrollo de una batería de múltiples dientes minúsculos que sirvió estructuralmente como base para la generación del pico de las formas más modernas (Pérez-Moreno et al., 1994). El yacimiento de Las Hoyas ha proporcionado un relativamente abundante registro de terópodos avianos , de los que, hasta el momento se han descrito tres géneros de enantiornitas: Iberomesornis, Concornis y Eoalulavis (Sanz et al., 1988; Sanz y Bonaparte, 1992; Sanz y Buscalioni, 1992; Sanz y Ortega, 2002;) (fig. 3c ). ...
Article
Full-text available
Body fossils of the Iberian Peninsula dinosaurs are very relevant for the knowledge of several aspects of the evolutionary history of the group, and, in addition, for the interpretation of the distribution of many of its components, due to the geographic situation of the Iberian Peninsula. Almost all of the groups of dinosaurs are represented in the Iberian Peninsula record: ornithopods, thyreophorans, theropods and sauropods. These groups are present, mainly, in the transit Jurassic-Cretaceous (Kimmeridigian- Berriasian), the upper part of the Lower Cretaceous (Barremian-Aptian) and in the end of the Upper Cretaceous (Campanian-Masstrichtian). Ornithischian dinosaurs are represented by thyreophorans such as the stegosaurians Dacentrurus and Stegosaurus, the ankylosaurs Dracopelta, Polacanthus and Struthiosaurus, and ornithopods like hypsilophodontids, basal iguanodontians (Rhabdodon), dryosaurids, camptosaurids (Draconyx and Camptosaurus), iguanodontids (Iguanodon) and hadrosaurids (Pararhabdodon). Some Incertae sedis and taxa in process of description are present too. Sauropods are represented by taxa related to Neosauropoda (Lourinhasaurus, Dinheirosaurus, Galveosaurus and Losillasaurus) and titanosauriforms (Aragosaurus, Lusotitan and Lirainosaurus). In addition, new forms are still in description, like the sauropods of Riodeva (Teruel), Peñarroya de Tastavins (Teruel) and Morella (Castellón). Theropods are represented by the ceratosaurian Ceratosaurus, the spinosauroid Torvosaurus, the carnosaurs Lourinhanosaurus and Allosaurus, the tyrannosaurid Aviatyrannis, the ornithomimosaur Pelecanimimus, and the avian-theropods Iberomesornis, Concornis, Eoalulavis and Noguerornis. Nevertheless, theropods diversity is more abundant as it shows the great variability of teeth morphotypes identified. registro de restos directos de dinosaurios en la Península Ibérica ha mostrado, en los últimos años, que puede ser muy relevante para el conocimiento de distintos aspectos de la historia evolutiva del grupo y, dada la posición de la Península Ibérica, para la interpretación de la distribución de muchos de sus componentes. El registro ibérico cuenta con representantes de casi todos los grandes grupos de dinosaurios: ornitópodos, tireóforos, terópodos y saurópodos, que están bien representados, sobre todo en el tránsito Jurásico-Cretácico (Kimmeridgiense-Berriasiewe), en parte del Cretácico Inferior (Barremiense-Aptiense) y en el final del Cretácico Superior (Campaniense-Maastrichtiense). El conjunto de ornitisquios está compuesto por tireóforos, de los que se han identificado dos estegosaurios (Dacentrurus y Stegosaurus) y tres anquilosaurios (Dracopelta, Polacanthus y Struthiosaurus) y ornitópodos: hipsilofodóntidos, iguanodontia basales (Rhabdodon); driosáuridos, camptosáuridos (Draconyx y Camptosaurus), iguanodontoideos (Iguanodon) y hadrosáuridos(Pararhabdodon). Además existe un gran número de formas de asignación dudosa o aún por describir. El registro de saurópodos está fundamentalmente compuesto por formas cercanas al nodo Neosauropoda (Lourinhasaurus, Dinheirosaurus, Galveosaurus y Losillasaurus) y titanosauriformes (Aragosaurus, Lusotitan y Lirainosaurus), además de una serie de formas nuevas en fase de descripción, como los saurópodos de Riodeva (Teruel), Peñarroya de Tastavins (Teruel) y Morella (Castellón). El conjunto de géneros de terópodos ibéricos está constituido por el ceratosaurio Ceratosaurus, el espinosauroide Torvosaurus, los carnosaurios Lourinhanosaurus y Allosaurus, el tiranosauroide Aviatyrannis, el ornitomimosaurio Pelecanimimus, y los terópodos avianos Iberomesornis, Concornis, Eoalulavis y Noguerornis. Sin embargo, la diversidad de terópodos es mucho mayor, como muestra la abundante colección de morfotipos dentarios identificados.
Article
Full-text available
Recent cladistic analyses have placed the Early Cretaceous avian, Iberomesornis romerali, outside the enantiornithine radiation at the base of Ornithothoraces. This conclusion is based on erroneous interpretations of the holotypic skeleton, which is shown here to exhibit ten enantiornithine synapomorphies. Revised diagnoses are presented for Enantiornithes and Iberomesornis romerali, which is very close in skeletal form to the Spanish and Chinese enantiornithines Concornis lacustris and Sinornis santensis, respectively.
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The evolution of avian flight can be interpreted by analyzing the sequence of modifications of the primitive tetrapod locomotor system through time. Herein, we introduce the term "locomotor module" to identify anatomical subregions of the musculoskeletal system that are highly integrated and act as functional units during locomotion. The first tetrapods, which employed lateral undulations of the entire body and appendages, had one large locomotor module. Basal dinosaurs and theropods were bipedal and possessed a smaller locomotor module consisting of the hind limb and tail. Bird flight evolved as the superimposition of a second (aerial) locomotor capability onto the ancestral (terrestrial) theropod body plan. Although the origin of the wing module was the primary innovation, alterations in the terrestrial system were also significant. We propose that the primitive theropod locomotor module was functionally and anatomically subdivided into separate pelvic and caudal locomotor modules. This decoupling freed the tail to attain a new and intimate affiliation with the forelimb during flight, a configuration unique to birds. Thus, the evolution of flight can be viewed as the origin and novel association of locomotor modules. Differential elaboration of these modules in various lineages has produced the diverse locomotor abilities of modern birds.
Article
Concornis lacustris gen. et sp. nov. is a new fossil bird from the Early Cretaceus (Barremian) of Las Hoyas, Cuenca, Spain. Concornis is roughly twice the size of Iberomesornis, the first bird described from Las Youas, but it is not the adult of the latter. Concornis is more derived than Iberomesornis, with a true tibiotarsus and a fan-like distal metatarsal zone with distinct trochlear structures. Concornis is one of the closer known sister taxa of the Ornithurae. This sister group plus Iberomesornis form the clade Euornithes, diagnosed by a strut-like coracoid, a derived avian furcula and a pygostyle. There is increasing evidence for an adaptive radiation of birds during the Early Cretaceous. After feathers appeared, the first stage of the radiation was the rapid evolution of active flight structures. Based on a "legginess index' in extant birds, an aquatic habit is suggested for Las Hoyas birds. -from Authors
Article
The evolution of avian flight can be interpreted by analyzing the sequence of modifications of the primitive tetrapod locomotor system through time. Herein, we introduce the term "locomotor module" to identify anatomical subregions of the musculoskeletal system that are highly integrated and act as functional units during locomotion. The first tetrapods, which employed lateral undulations of the entire body and appendages, had one large locomotor module. Basal dinosaurs and theropods were bipedal and possessed a smaller locomotor module consisting of the hind limb and tail. Bird flight evolved as the superimposition of a second (aerial) locomotor capability onto the ancestral (terrestrial) theropod body plan. Although the origin of the wing module was the primary innovation, alterations in the terrestrial system were also significant. We propose that the primitive theropod locomotor module was functionally and anatomically subdivided into separate pelvic and caudal locomotor modules. This decoupling freed the tail to attain a new and intimate affiliation with the forelimb during flight, a configuration unique to birds. Thus, the evolution of flight can be viewed as the origin and novel association of locomotor modules. Differential elaboration of these modules in various lineages has produced the diverse locomotor abilities of modern birds.