scholarly journals A multi-proxy assessment of terrace formation in the lower Trinity River valley, Texas

2021 ◽  
Author(s):  
Hima J. Hassenruck-Gudipati ◽  
Thaddeus S. Ellis ◽  
Timothy A. Goudge ◽  
David Mohrig

Abstract. A proposed null hypothesis for fluvial terrace formation is that internally generated or autogenic processes such as lateral migration and river-bend cutoff produce variabilities in channel incision that lead to the abandonment of floodplain segments as terraces. Alternatively, fluvial terraces have the potential to record past environmental changes from external forcings that include temporal changes in sea-level and hydroclimate. Terraces in the Trinity River valley have been previously characterized as Deweyville groups and interpreted to record episodic cut and fill during late Pleistocene sea-level variations. Our study uses high-resolution topography of a bare-earth digital elevation model derived from airborne lidar surveys along ~88 linear km of the modern river valley. We measure both differences in terrace elevations and widths of paleo-channels preserved on these terraces in order to have two independent constraints on terrace formation mechanisms. For 52 distinct terraces, we quantify whether there is a clustering of terrace elevations – expected for allogenic terrace formation tied to punctuated sea-level and/or hydroclimate change – by comparing variability in a chosen set of terrace elevations against variability associated with randomly selected terrace sets. Results show Deweyville groups record an initial valley floor abandoning driven by allogenic forcing, which transitions into autogenic forcing for the formation of younger terraces. For 79 paleo-channel segments preserved on these terraces, we connected observed changes in paleo-channel widths to estimates for river paleo-hydrology over time. Our measurements suggest the discharge of the Trinity River has changed systematically by a factor of ~2 during the late Pleistocene. Methods introduced here combine river-reach scale observations of terrace sets and paleohydrology with local observations of adjacent terrace-elevation change and paleo-channel bend number to show how interpretations of allogenic versus autogenic terrace formation can be evaluated within a single river system.

2019 ◽  
Vol 10 (1) ◽  
Author(s):  
Pedro Michelutti Cheliz ◽  
Regina Celia Oliveira

This paper presents a geomorphological, pedological and geochronological characterization and contextualization of geomorphogenetic, chronomorphological and environmental sequences from the Araraquara area (central São Paulo State, Southeast Brazil), and their relationship to lithic material from hunter-gatherer archaeological lithic sites. A special emphasis is given to a detailed study of the lowlands of the Jacaré-Guaçu River (between the cities of Araraquara and Boa Esperança do Sul, São Paulo state, Brazil), near the Boa Esperança II hunter-gatherer archaeological site, BES II, in an area of clear asymmetry of the alluvial plain and adjacent slopes. Data derived from the survey of estimated morphogenetic and environmental dynamics are used to contextualize the archaeological material of the BES II site, which is discussed as being associated with the Pleistocene-Holocene transition (an unusual occupation age for the Brazil southeast). We pointed to alternation between successions linked to a quaternary manifestation of a longer pattern of changes of lateral flatting processes and stability of base level with others linked to vertical incision and adequacy to a new base level. We propose a geomorphological model for the Lowlands of Jacaré-Guaçu River, highlighting the possibility that the asymmetry of the plain would be linked to a wider heterogeneity of its geomorphological context of semidetails, partially correlated with the overlapping of neotectonic influence and environmental fluctuations. It is suggested that data from the physical environment of the above mentioned lowlands are compatible with absolute ages obtained by OSL (lower terrace Ia, 14,500±3000 years BP, basal gravel level of the surface coverings, to 10,900±1500 and 4090±340 years BP at the sandy soils and sediments above the gravel) and 14C (8630 years BP, at the level of gleyed sandy-clay soil of 120 cm deep of the low terraces IIa) on archaeological levels of the low terraces of the Jacaré-Guaçu river, in a context of climatic transition from semi-arid conditions to higher humidity, hydrological changes (ephemeral and torrential channels changing to oscillating regimes of perennial channels, with sets of meanders of variable widths of paleochannels, suggesting climatic changes related to the modifications of the fluvial patterns), successive fluctuations (< 10 m) of base levels and large (500 m) lateral migration of the main river to the north guiding the local chronomorphological successions between Late Pleistocene and Late Holocene. The landscape and fluvial dynamics changes over time has influenced the availability of attributes needed for the hunter-gatherer lifestyle (such as fluctuations in the deposition/exposure of river pebbles used as raw material for tool making). Those oscillations are presented as a contribution to explain alternation between more and less dense archaeological levels along the vertical cuts of the low terraces and the location of exception of the BES II site (installed on a fluvial plain and low terraces in a segment characterized by the rarity of rocky outcrops, while most sites in the Araraquara area are linked to slopes, proximal to rocky outcrops - primary sources of lithics artifacts making) on the geomorphological Araraquara area context 


2012 ◽  
Vol 62 (4) ◽  
pp. 561-580 ◽  
Author(s):  
Ewa Świerczewska-Gładysz

ABSTRACTŚwierczewska-Gładysz, E. 2012. Hexactinellid sponge assemblages across the Campanian-Maastrichtian boundary in the Middle Vistula River section, central Poland. Acta Geologica Polonica, 62 (4), 561-580. Warszawa.The sponge fauna from the Upper Campanian-lowermost Maastrichtian succession of the Middle Vistula River valley (central Poland) is represented mainly by dictyid hexactinellid sponges (Hexactinosida and Lychniscosida). Their greatest abundance and taxonomic variability is noted in the “Inoceramus” inkermanensis Zone (Upper Campanian), and they are less diverse in the overlying (Upper Campanian) Trochoceramus costaecus Zone and lower “Inoceramus” redbirdensis Zone. In the upper “Inoceramus” redbirdensis Zone (basal Maastrichtian in the sense of the Tercis rather than the Boreal definition) they are extremely rare. With the beginning of the Maastrichtian the number of dictyid sponges gradually increases.The observed changes in the abundance and taxonomic variability of the dictyid sponges indicate environmental changes in the latest Campanian-earliest Maastrichtian sea in the area. It seems that changes in basin bathymetry, confined to eustatic sea-level changes in the latest Campanian and early Maastrichtian, were the most important factor. Progressive shallowing of the basin in the latest Campanian drastically restricted the development of dictyids. In the peak regression, the sea level could have fallen to only several tens of metres. The gradual recovery of the sponge assemblages correlates with subsequent deepening of the basin with the start of the Maastrichtian


The transition from late interglacial (temperate) to early glacial (cold) stage environments, involving not only climatic deterioration, but also a fall in sea level, has been rarely described. The Cotentin Peninsula, Normandy, lies beyond Pleistocene ice limits, and hence has less stratigraphic complexity than areas characterized by ice advances and retreats. Furthermore, it possesses a number of closely spaced coastal sites where late interglacial to early glacial organomineral sediments are present. These sediments overlie interglacial raised beach deposits, or more ancient wavecut rock platforms, and are succeeded by periglacial (head and loess) deposits. These localities thus afforded an ideal opportunity for detailed multidisciplinary studies of sea level and terrestrial environmental change. Investigation of the geomorphology and stratigraphy was accompanied by palaeobotanical and palaeoentomological analysis of the organomineral deposits. The fossil evidence shows that as sea level fell from a height similar to the present day, the climate cooled from temperate to arctic, and that these changes were accompanied by major modifications in the flora and fauna. Previous stratigraphic, pedological and palynological studies of the sites have been taken to imply multiple environmental changes, with ages ranging from Elsterian to Weichselian. The research described here, together with radiometric age determinations, implies that the raised beach and organomineral sediments were associated with a single marine regression between ca . 121 and 45 ka, that is, late in the Eemian Interglacial and early in the Weichselian Glacial stage. These environmental changes are discussed with reference to those recorded at sites in France and Britain that probably date from the same period.


2021 ◽  
Author(s):  
Jacob Burstein ◽  
John Goff ◽  
Sean Gulick ◽  
Christopher Lowery ◽  
Patricia Standring ◽  
...  

Understanding how barrier islands respond to factors such as variations in sediment supply, relative sea-level rise, and accommodation is valuable for preparing coastal communities for future impacts of climate change. Increasingly, the underlying antecedent topography has been observed to have a significant control on the evolution of the barrier island system by providing increased elevation, decreased accommodation, and sediment supply for the barrier to rework and anchor upon. However, less attention has been focused on how back barrier sediments respond to this decreased accommodation, and how this may affect barrier island evolution. Additionally, the control in which the geometry of the underlying valley itself has on the initiation of barrier islands is poorly understood. Here we examine the stratigraphic framework of the Trinity River incised valley, offshore Galveston, Texas in order to investigate the role of antecedent topography in the evolution of an ancient barrier island system. We present high-resolution imaging of the Trinity incised valley fill using over 1200 km2 of 3D seismic, <700 km of 2D envelope and full waveform chirp data, along with 2 piston cores, 4 gravity cores, 1 platform boring, with associated grain size, foraminiferal, and radiocarbon data. We find that the geometry and elevation of the underlying antecedent topography plays a central role in the evolution of the barrier island system, promoting both initiation and stabilization. This study provides a methodology to investigate the evolution of a relict barrier island system where little to none of the barrier is preserved. With this methodology, we revise the established Holocene paleoshoreline model for the Trinity incised valley.


Author(s):  
Nikolay N. Lashchinskiy ◽  
◽  
Olga Yu. Pisarenko ◽  

Spruce forests of the Tuva Republic are not sufficiently described in literature. Spruce forests occupy small areas, but they are characterized by high species diversity. Enclaves of forest communities outside the forest belt are particularly interesting. The actual problem concerns species composition which forms plant communities existing under environmental and climate conditions that are not favorable for it. The aim of the research is to describe the communities of the valley dark coniferous forests in the model river valley in Central Tuva, to assess their diversity, to analyze species composition and to identify the main factors determining it. In the course of the fieldwork in 2020, we examined coniferous forests along the Koptu river, on the southern slope of the Academic Obruchev range (See Figures). In this part of the range, the foothills are occupied by steppe vegetation; forest-steppe landscapes prevail at altitudes of 800-1000 m; above there is the taiga belt, the upper border of the forest is about 1900 m above sea level. Two key areas were investigated; one of them is located in the middle course of the river within the taiga belt (51.90- 51.92°N; 95.45-95.48°E, 1400-1500 m above sea level), the other is in the lower course of the river in the forest-steppe belt (51.55-51.70°N; 95.34-95.45°E, 700-900 m above sea level). In total, 11 relevés were made on plots of 20×20 m by the standard method. We established that the forests are rich in species: 98 taxa were registered (See Table). It could be expected that coniferous forests in the river valley within the forest-steppe belt are a continuation of the above located communities, a continuation of communities from the taiga belt. However, our materials have demonstrated that it is not so. We revealed that, despite the physiognomic similarity, the dark coniferous communities growing in the river valley in its lower course differ significantly from those growing within the taiga belt (See Table). Larix sibirica is abundant everywhere; but in the taiga belt Pinus sibirica dominates in the valley communities, and Picea obovata prevailes in the river valley in the forest-steppe belt. Apart from it, the communities of these two key sites differ significantly in their species composition. Analysis of the ecology of differentiating species shows that the difference is due to a complex of factors. Four groups of species can be distinguished in the investigated forests: I. Taiga species which are only encountered in forests of the upper part and are absent below (Aegopodium alpestre, Carex iljinii, Cerastium pauciflorum, Vaccinium vitis-idaea, V. uliginosum). II. Meadow species, symmetrically, only occur in the forests of the lower part and are absent in the taiga belt (Galium boreale, Lathyrus pratensis, Rubus saxatilis and Vicia cracca, Achillea asiatica, Adonis sibirica, Artemisia laciniata, Iris ruthenica). The two groups mentioned above reflect the difference in altitude as well as the influence of the zonal environment. III. A series of species in the downstream valley forests reflect a waterlogging process, which takes place there due to the altitudinal gradient declining and surface flattening (Angelica tenuifolia, Caltha palustris, Carex cespitosa, C. dioica, Equisetum scirpoides, Delphinium crassifolium, Galium uliginosum, Lathyrus palustris, Parnassia palustris, Ribes procumbens; among mosses – Calliergonella cuspidata, Helodium blandowii, Timmia megapolitana, Tomentypnum nitens). IV. A number of species with mainly taiga or Arctic-Alpine distribution were recorded only in larch-spruce forests in the river valley in the forest-steppe belt and they are absent in the forests of the upper key area (Carex alba, Bistorta vivipara, Carex sedakowii, Orthilia obtusata, Pedicularis sceptrum-carolinum, Saussurea alpina, Schizachne callosa). For these species, it is impossible to explain their presence in the forest-steppe belt by modern ecological conditions. Their presence in the valley spruce forests has historical reasons and could be caused by the conditions of the Late Pleistocene cooling. So, we can draw a conclusion that the massif of valley spruce forests in the lower part of the Koptu river is a relict community formed in the Late Pleistocene periglacial environment on permafrost soils. In present conditions, it is in unstable equilibrium. The massif is the habitat of a number of rare species. In particular, the Orchidaceae taxa were found here, four of which are included in the Red Book of the Republic of Tuva (Cypripedium calceolus, Dactylorhiza sibirica, Epipogium aphyllum, Neottianthe cucullata). The valley forest of the lower part of the Koptu river can be nominated as a high conservation value forest and recommended to be included in the list of the Important Plant Areas of the Altai-Sayan region. The massif is under the strong anthropogenic pressure; in order to avoid extinction, it needs to be protected.


The Jewett Mine is a ca. 21, 000-acre lignite mine in the post oak savannah of Freestone, Leon, and Limestone counties, Texas. The project area straddles the divide between the Navasota River valley on the west and the Trinity River valley on the east and lies at the western margin of the Caddoan area . Although residential use of the area by the Caddo has not been documented, many sites have yielded small quantities of Caddoan pottery, and it is likely that cultures indigenous to the region were affected by the development of Caddoan culture not far to the east. For reference, the George C. Davis Site (41CE19) lies only 95 km to the east-northeast. In addition to contributing information about the interaction between Caddoan and neighboring groups in the central part of East Texas, the Jewett Mine sites, by virtue of their location in the Eastern Woodlands but outside of the Caddoan area proper, have the potential to shed light on such topics as regional Caddoan settlement systems and the origins of Caddo culture.


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